Specialist Climate Change Assessment Report For the proposed
Musina-Makhado Special Economic Zone South Site
Musina-Makhado Special Economic Zone (SOC) Limited Limpopo Economic Development Agency
September 2021
Executive Summary This report sets out a climate change impact assessment for the planned Musina-Makhado Special Economic Zone (SEZ). The analysis is based on the judgement in the Thabametsi court case where the court found that environmental impact assessments should consider both the potential impact of a proposed project on climate change, as well as the potential impact of climate change on the proposed project. The analysis presented in this report considered the climate change impacts of the project in the context of both South Africa’s domestic legal environment as well as the international commitments the country has made. The report builds on a 2°C target and will fall short in its recommendations if a 1.5°C target is set, as is envisaged in the Paris Agreement. In conclusion, this project presents a unique challenge. When considered from a South African National perspective, the impacts of the project are: • The project has a High (negative) impact rating for the operational phase of the project, in terms of the 2014 NEMA EIA Regulations, with a significance score of 100. • The emissions released by the various activities associated with the SEZ over the operational lifetime of the project will consume as much as 10% of South Africa’s carbon budget. The impact on the emission inventory of the country is therefore VERY HIGH (negative). • When considering the impact score for the construction phase, the impact score will be High. This is independent of the magnitude of the GHG emissions. However, these emissions pale in comparison to the operational emissions that will result from the proposed SEZ and various activities planned within. • Although the impact of the activities associated with operational phase of the SEZ is considered to be HIGH with a magnitude impact (in terms of the specialist climate change assessment methodology) of VERY HIGH in terms of the country’s emission inventory, such impact has been considered within the context of the provisions of the Thabametsi case, as well as the relevant regulatory requirements relating to South Africa’s energy sector, climate change commitments and social context. o The contextual consideration of the project aligns with the requirements of Section 240(1) of NEMA which provides that the Minister must comply with the Act, and must “take into account all relevant factors.” At the time of drafting the report, the IRP 2010-2030 was the binding policy determining South Africa’s electricity mix. o However, since the adoption of the IRP 2010, South Africa has made numerous climate change commitments in its NDC, and as such, the IRP 2010 is premised on facts that are outdated when considering more recent policy developments and commitments. • Therefore, environmental authorisation of the thermal coal fired power plant cannot be granted merely based on the fact that the IRP 2010 allows for energy to be procured from coal. Additional factors such as the project’s overall impact in relation to other factors such as South Africa’s NDC and South Africa’s Peak Plateau Decline (PPD) emission trajectory must be considered. 2
Based on the above, and considering the relevant regulatory factors which includes, but is not limited to South Africa’s Nationally Determined Contribution (NDC), the Peak Plateau Decline (PPD) emission trajectory as well as the outdated nature of the Integrated Resource Plan 2010, the various activities planned as part of the SEZ should not be implemented, unless the following can be met: • If the individual processes within the SEZ are built according to the SBTi intensities identified in the report (see Table 14), then emissions of the project could be reduced by approximately 10 million tonnes per year, to a total emissions of 24 million tonnes per year. In the light of the above, the recommendations in the report are: • Environmental authorisations for the individual plants in the SEZ should only be granted if the following emission intensities can be achieved: Plant Coke Plant Ferrochrome plant Ferromanganese plant Silicon-manganese plant Carbon steel plant Stainless steel plant Lime plant Cement plant Sewage treatment plant Water treatment plant
• •
•
•
2°C target intensities for 2030 0.21 tCO2e/tonne product 3.37 tCO2e/tonne product 3.37 tCO2e/tonne product 5.18 tCO2e/tonne product 0.37 tCO2e/tonne product 0.78 tCO2e/tonne product 0.87 tCO2e/tonne product 0.80 tCO2e/tonne clinker 0.0005 tCO2e/tonne water
0.0005 tCO2e/tonne water
In addition, the environmental authorisation should require a re-assessment of the emission intensities 5 years after the start of operation of the respective plants The construction of a coal fired thermal power plant should not be approved unless the plant is fitted with a carbon capture and storage unit that can sequester ALL emission from the combustion of coal from the starting date of operation. Without CCS, the coal fired power station will severely reduce South Africa’s ability to achieve its NDC. We make this recommendation in the context of the comment regarding the lack of feasibility of CCS as described in Section 4.1.3). In practical terms this means that approval for the coal fired thermal power plant should, in our opinion, not be granted. The Specialist studies (groundwater, surface water, etc.) for the environment authorisation for each plant in the overall SEZ should specifically address the impact of climate change on each area. For example, the ground water study should address the impact of climate change on the recharge of groundwater, etc. This is also important for all studies related to the social impacts of the projects. Water is of critical concern. The study area is already severely water stressed and climatic modelling for the area indicates increased ambient temperatures, prolonged periods of drought and greater rainfall variability. These factors will exacerbate current water risks, both in South Africa and in neighbouring Zimbabwe. The impacts of climate change, as 3
•
•
well as the potential changes in climatic parameters have, a broader impact on water sources than the immediate zone of influence. Current water stress in the region is anticipated to be exacerbated by climate change impacts. The area is anticipated to become increasingly hotter and drier, thus the water availability in the area may critically constrained resulting in water shortages affecting the region in its entirety. Thus, any approval of the project should be conditional upon an overall water risk analysis of the region (Limpopo Province) being conducted, with specific reference to the proposed SEZ project. This is to identify the broader water stress and possible pollution risks posed by the proposed SEZ, which will be exacerbated by the impacts of climate change in the Province. It is advised that a regional perspective be developed with regards to water resources in the Province, current land use change patterns, existing water uses and climate change. This will allow for more informed decision-making related to the development of the proposed SEZ. The provision of water will rely on an international supply of water from Zimbabwe. Any approval of the project should be conditional upon a thorough assessment of how the diversion of this water will impact the climate change-related adaptive capacity of the affected communities in Zimbabwe. All indoor working environments should be well insulated and air conditioned and drinking water should be made readily available throughout the MMSEZ. This is to reduce the potential impacts of heat-related health impacts, such as dehydration, on the health of employees. The frequency and intensity of heat-related health impacts is predicted to increase as climate change progresses.
The potential impacts of climate change in this area, within the context of this project, such as increasing temperatures, prolonged periods of drought, flash foods from severe rainfall events, biodiversity and agricultural loss and significant water related constraints, could have significant impacts on the project itself as well as entrench the vulnerability of people in the area. This will increase poverty and prevent communities from building climate resilience, specifically in the long-term. This assessment was undertaken by Promethium Carbon under bid number LEDA/AIA/2018/19-2. The Scope of Work as proposed by the Service Level Agreement has been addressed as follows: Requirements as per Scope of Work Relevant Chapters of this report depicted in Service Level Agreement Review of legislation, policy Chapter 3 sets out the various relevant climate change schemes and frameworks related documents and strategies pertaining to climate applicable to the proposed change in terms of global, national, provincial and development local level. Baseline description of Chapter 3 provides an overview of the national, climate change landscape provincial and local context of climate change. Climate Resilience Chapter 6 discusses the impacts of climate change on Assessment the projects which is assessed in terms of exposure,
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Requirements as per Scope of Work Relevant Chapters of this report depicted in Service Level Agreement sensitivity and adaptive capacity to inform the proposed SEZ’s vulnerability risk rating. Climate baseline Chapter 3 discusses the nature of climate change, which includes reference to the pre-industrial era Climate change projections Chapter 3 discusses observed climate change trends and projections on a national. Provincial and local level. Impact Assessment: Chapter 5 provides the emission intensities of the Assessment of direct, proposed SEZ and a discussion on the related impact indirect, cumulative GHG on climate change. As the designs for the various emission impacts during the: activities and related plants envisaged for the SEZ in terms of their respective construction and • Construction phase decommissioning planning, have not yet been • Operational phase finalised, the emissions for each of these plants in • Decommissioning terms of these phases cannot yet be calculated. and rehabilitation Therefore, this assessment has determined emission phase intensities for the various operational activities envisioned within the SEZ (based on available information), required to achieve national and international climate change objectives. Emissions management Both Chapter 5 and Chapter 8 discusses emission measures mitigation measures. Proposed development’s Chapter 5 details the project’s direct impact on direct impacts on climate climate change. change Extent of GHG emissions to Chapter 5 details the emission intensities, assumed arise from the development for the SEZ. How climate change will impact on the project How predicted climate change effects on the environment at both national and local scale will be aggravated by the project’s impacts How impacts can be avoided, mitigated or remedied Assessment of social and environmental costs of the proposed development’s GHG emissions
Chapter 6 discusses the impacts of climate change on the project. Chapter 6 discusses the impacts of climate change on the project and the related exacerbation of project impacts as a result of climate change.
Both Chapter 5 and Chapter 8 discusses emission mitigation measures. Chapter 6 discusses the impacts of climate change on the project and the related exacerbation of project impacts as a result of climate change. These impacts are contextualised within the social and natural environment of the study area. Chapter 5 also provides a detailed assessment of the impact of the project in relation to South Africa’s carbon budget.
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Table of Contents Executive Summary .................................................................................................................................... 2 Table of Contents ....................................................................................................................................... 6 List of Figures.............................................................................................................................................. 9 List of Tables ............................................................................................................................................. 11 Declaration of Independence .................................................................................................................. 12 Details of Specialist................................................................................................................................... 13 List of Acronyms and Terms .................................................................................................................. 16 Key Terms and Definitions ..................................................................................................................... 17 Introduction ...................................................................................................................................... 18 1.1
Structure of the Report............................................................................................................ 21
Project Description .......................................................................................................................... 23 2.1
Regional Project Context ........................................................................................................ 23
2.2
Project Overview ...................................................................................................................... 24
2.2.1
Industry capacity and construction phasing ................................................................. 25
2.2.2
SEZ water demand .......................................................................................................... 26
2.2.3
Labour demand ................................................................................................................ 28
2.3
Project Setting ........................................................................................................................... 28
2.3.1
Location............................................................................................................................. 28
2.3.2
Land capability.................................................................................................................. 28
2.3.3
Water.................................................................................................................................. 29
2.3.4
Biodiversity ....................................................................................................................... 30
2.3.5
Settlements and surrounding communities .................................................................. 31
Climate Change Context.................................................................................................................. 33 3.1
Global Context ......................................................................................................................... 33
3.2
Local Context............................................................................................................................ 34 South Africa’s response to climate change................................................................... 34
3.2.2
South Africa’s carbon budget ......................................................................................... 35
3.2.3
Local climate change impacts ......................................................................................... 36 Pathways for a just transition for the Province of Limpopo ..................................... 36
3.3
Observed Trends and Projected Climate Change ............................................................... 37 National overview ............................................................................................................ 37 6
Provincial overview ......................................................................................................... 39 Municipal overview.......................................................................................................... 42 3.4
Other Potential Climate Change Dimensions Relevant to the SEZ................................. 44
Methodology ..................................................................................................................................... 45 4.1
Impacts of the Project on Climate Change .......................................................................... 45 Greenhouse gas emissions estimation methodology .................................................. 45 Environmental impacts of greenhouse gas emissions ................................................ 49
4.1.3 4.2
Carbon Capture and Storage .......................................................................................... 51
Impacts of Climate Change on the Project .......................................................................... 51
Impact of Project on Climate Change ........................................................................................... 55 5.1
Quantification of the Project’s Greenhouse Gas Emissions ............................................. 55
5.2
Impacts on Greenhouse Gas Inventories ............................................................................. 58
5.2.1
South African Context .................................................................................................... 58 Global Context ................................................................................................................. 60
5.3
Impacts on Climate Change.................................................................................................... 62
5.4
Project Alternatives .................................................................................................................. 64
Impacts of Climate Change on the Project................................................................................... 66 6.1
Emission scenarios and impact analysis ................................................................................ 67
6.2
Increased Temperature ............................................................................................................ 69
6.3
Water related impacts .............................................................................................................. 71 Water internationally ....................................................................................................... 71 Water locally ..................................................................................................................... 73 Physical risks within the value chain ............................................................................. 79 Disaster risks – flash flooding ........................................................................................ 80
6.4
Social Impacts ........................................................................................................................... 82 Description of local municipality socio-economic vulnerabilities ............................ 83 SEZ community vulnerability drivers ........................................................................... 86 Human Health .................................................................................................................. 88 Human settlements .......................................................................................................... 89 Water and sanitation ........................................................................................................ 90 In-migration risks ............................................................................................................. 90
6.5
The Natural Environment ...................................................................................................... 92
6.5.1
Land use cover change .................................................................................................... 93
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Biomes and ecosystem services ..................................................................................... 93 6.5.3
Considering the biodiversity in relation to climate adaptation .................................. 95 Drought ............................................................................................................................. 96
6.6
Transitional Risks ..................................................................................................................... 96
6.7
Summary of climate change resilience assessment .............................................................. 98
Climate Change and the Possibility of Stranded Assets............................................................ 102 Mitigation and Adaptation ............................................................................................................ 105 8.1
Design considerations............................................................................................................ 105
8.2
Operational Emissions Management .................................................................................. 106
Opinion on the Project .................................................................................................................. 107
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List of Figures Figure 1: Musina-Makhado Special Economic Zone Proposed Location4. .................................................... 24 Figure 2: EMSEZ Site water balance7. ................................................................................................................... 27 Figure 3: SEZ total labour figures7. ........................................................................................................................ 28 Figure 4: Land cover 4. .............................................................................................................................................. 29 Figure 5: Vhembe Biosphere Reserve4 . ................................................................................................................. 31 Figure 6: Percentage of households in informal dwellings in the Vhembe District Municipality12 .............. 32 Figure 7: Projected Southern African temperature change under RCP4.526. ................................................... 38 Figure 8: Projected precipitation change for South Africa under different emissions scenarios26 ............... 39 Figure 9: Limpopo drought tendencies for the period 1995-2024. ................................................................... 40 Figure 10: Flood Hazard index27. ............................................................................................................................ 42 Figure 11: Proposed Methodology boundary and input...................................................................................... 46 Figure 12: Vulnerability assessment process.......................................................................................................... 53 Figure 13: Emissions per project type for the 30 year life of the project ......................................................... 57 Figure 14: Effect of the project on the IRP .......................................................................................................... 60 Figure 15: The growing role of steel for a low carbon future (2DS - 2˚C scenario. 4DS - 4˚C scenario, 6DS - 6˚C scenario). .................................................................................................................................................. 61 Figure 16: Climate risks impacting various sectors (adopted) ............................................................................ 66 Figure 17: Forward looking scenario analyses ....................................................................................................... 68 Figure 18: Projected average temperate change for the period 2021 -2050, relative to the baseline period (1961 – 1990)27. .......................................................................................................................................................... 69 Figure 19: Projected change in the number of very hot days (>35˚C) for the period 2021 -2050, relative to the baseline period (1961 – 1990)27. ........................................................................................................................ 70 Figure 20: Projected change in drought tendencies for the period 2035 - 2064, relative to the baseline period (1986 – 2005) under the low mitigation scenario RCP 8,527. ................................................................. 74 Figure 21: Projected change in average rainfall for the period 2021 -2050, relative to the baseline period (1961 – 1990)27. .......................................................................................................................................................... 75 Figure 22: Projected change in extreme rainfall days under RCP 8.5 for the year 205027.............................. 76 Figure 23: SEZ - overall water stress52. .................................................................................................................. 77 Figure 24: SEZ - upstream storage52....................................................................................................................... 78 Figure 25: SEZ - inter annual variability52.............................................................................................................. 79 Figure 26: Overall water stress in Mpumalanga region52. .................................................................................... 80 Figure 27: Disaster incidences from 2016 - 2018. ................................................................................................ 81 Figure 28: Percentage of households in informal dwellings in the Vhembe District Municipality12. .......... 83
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Figure 29: Population living in poverty. ................................................................................................................. 85 Figure 30: Vhembe district Municipality Percentage of Young (<5yrs) and elderly (>64yrs)12. ................... 89 Figure 31: Summary of the climate-related events per country in southern Africa since 1980..................... 91 Figure 32: Bioclimatic envelope projections to 205022. ....................................................................................... 94 Figure 33: Comparison of the global 2°C carbon budget with fossil fuel reserves CO2 emissions potential. ..................................................................................................................................................................................... 103 Figure 34: Shortfall in country level contributions to meet the 2⁰C target. ................................................... 104 Figure 35: Global levelized cost of electricity from utility-scale renewable power generation technologies, 2010-2017. ................................................................................................................................................................. 105
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List of Tables Table 1: Summary of Proposed Projects for SEZ ................................................................................................ 21 Table 2: Summary of Proposed Projects for SEZ ................................................................................................ 25 Table 3: Construction phase timeframes7 .............................................................................................................. 26 Table 4: Current and future water balance of Musina area with interventions. ............................................... 30 Table 5: Vhembe District Municipality key climate change vulnerability indicators12.................................... 43 Table 6: Emission intensity benchmarks used ...................................................................................................... 48 Table 7: Emission intensities required to achieve the Paris Agreement 2°C goal .......................................... 49 Table 8: Environmental impact assessment criteria ............................................................................................ 49 Table 9: Greenhouse gas emissions impact rating ................................................................................................ 50 Table 10: Musina Makhado SEZ Climate Change Risk and Vulnerability Analysis Components ............... 54 Table 11: Emissions provided in the Greenhouse Gas Emission Indicator Report ..................................... 55 Table 12: Annual project emissions ....................................................................................................................... 56 Table 13: The Musina-Makhado SEZ development's emissions relative to South Africa's carbon budget 58 Table 14: Comparison of current and required emission intensities. ................................................................ 61 Table 15: Climate change impacts of the Musina-Makhado SEZ Development emissions during operations .................................................................................................................................................................... 62 Table 16: Emission intensity comparison .............................................................................................................. 64 Table 17: Potential source of water in Zimbabwe10 ............................................................................................. 71 Table 18: Limpopo development level catchment water balances, 2010.......................................................... 73 Table 19: Vhembe District Municipality key demographic information (2011)12. .......................................... 84 Table 20: Climate change manifestation, community impacts and operational influence ............................. 87 Table 21: Potential impact analysis for the SEZ under RCP8.5......................................................................... 98
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Declaration of Independence The authors of this report do hereby declare their independence as consultants appointed by Deltabec Consulting to undertake a climate change assessment for the proposed SEZ. Other than fair remuneration for the work performed, the specialists have no personal, financial business or other interests in the project activity. The objectivity of the specialists is not compromised by any circumstances and the views expressed within the report are their own.
Robbie Louw
Karien Erasmus
Matthias Rommelspacher
Kenneth Slabbert
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Details of Specialist Promethium Carbon Promethium Carbon is a South African climate change and carbon advisory company based in Johannesburg. Our aim is to make a difference in climate change in Africa and our team of climate change professionals and technical experts assists businesses, ranging from small enterprises to multinational entities, on their journey towards a low carbon economy. We also assist governments and government institutions in planning for the imminent global carbon-constrained environment. We act as trusted advisors to our clients and have established ourselves as knowledge leaders in the climate space through our participation on various working groups and standards boards. We have been active in the climate change and carbon management space since 2004. Our client base includes many of the international mining houses and industrial companies that are operating in, and from, South Africa. Promethium Carbon’s climate change impact studies typically include an estimation of the carbon footprint of the activity or group of activities, as well as the vulnerability of the activity/ies to climate change. Promethium Carbon has calculated greenhouse gas inventories for over 60 entities and is proficient in applying the requirements of ISO/SANS 14064-1 and the Greenhouse Gas Protocol’s accounting standards, as well as South Africa’s greenhouse gas reporting guidelines. Promethium Carbon has also assisted around 40 clients develop climate change risk assessments, which includes the compilation of climate change specialist reports. Promethium Carbon’s assessments include thorough analysis of historical and projected weather data specific to the region in which the client operates. Promethium Carbon’s assessment of vulnerability goes beyond core operations to include impacts within the supply chain and broader network of the client. We have also conducted climate change risk and vulnerability assessments as part of the Carbon Disclosure Project for over 20 clients, many whom have reported annual since 2008.
Robbie Louw
is the founder and director of Promethium Carbon. He has over 15 years of experience in the climate change industry. His experience (35 years) includes research and development activities as well as project, operational and management responsibilities in the chemical, mining, minerals process and energy fields. Robbie is currently a member of The Southern African Institute of Mining and Metallurgy, Robbie’s experience in climate change includes (but is not limited) to: •
Climate change risk and vulnerability assessments for large mining houses.
•
Extensive experience in carbon foot printing. The team under his leadership has performed carbon footprint calculations for major international corporations operating complex businesses in multiple jurisdictions and continents.
•
Carbon and climate strategy development for major international corporations.
•
Climate change risk assessments for various companies and projects.
•
Climate change scenario planning and analysis, particularly in terms of the recommendations of the Taskforce on Climate-related Financial Disclosure. 13
Karien Erasmus is a principal climate change advisor at Promethium Carbon and holds an Honours Degree in Sustainable Development. Her postgraduate qualifications include diplomas in: Project management, community development and mine closure and ecological rehabilitation. She has been involved in the sustainability and climate change industry for the past 13 years, working extensively in Africa and on strategic local projects such as the Gautrain and the Bus Rapid Transit system in Johannesburg. Karien joined Promethium Carbon in 2015 and utilises her developmental background to inform the social context of various climate change and low carbon development projects. Karien holds memberships with the Land Rehabilitation Society of Southern Africa and International Association for Impact Assessment. Over the past three years Karien has worked extensively within the mining sector. Karien’s experience in climate change includes: •
Climate change risk and vulnerability assessments;
•
Climate change impact assessments as part of the Environmental Authorisation process;
•
Drafting Carbon Disclosure Project Climate Change and Water responses;
•
Assessment of climate change and energy related regulations;
•
Developing the land, community and energy nexus concept which links land rehabilitation to community upliftment through sustainable energy projects.
Matthias Rommelspacher is a Climate Change Advisor appointed at Promethium Carbon who
holds a Master’s in Environmental Engineering. His postgraduate studies focused on urban water management, air quality control, waste management and ecological systems design. Part of his studies included field work on Mahé in Seychelles, where he was part of a transdisciplinary team that assessed the waste management system of Mahé Island. The research for his thesis combined his background as a Chemical Engineer with his studies and focused on the processing of urban wastewater for nutrient recovery. Over the past several months at Promethium Carbon, Matthias has gained valuable experience. Some of the projects he has been active in include: •
Climate change impact assessments for major energy and gas installations;
•
GHG Reporting;
•
Climate change risk and vulnerability assessments; and
•
Calculations of various first principle concepts for modelling purposes, including: o Carbon tax models, o Carbon footprints, and o Science-Based Target models.
Kenneth Slabbert is a climate change advisor at Promethium Carbon and holds a Bachelor of Engineering in Mechanical Engineering. Kenneth joined Promethium Carbon in 2018 and has been working in the climate change industry for the past 1.5 years. Kenneth’s experience in climate change includes: •
Carbon footprint / Greenhouse gas inventory development
•
Energy efficiency studies 14
•
Data analysis
•
Climate Change Impact Assessments
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List of Acronyms and Terms Abbreviation
Definition
SEZ
Special Economic Zone
CO2
Carbon dioxide
CH4
Methane
IPCC
Intergovernmental Panel on Climate Change
IRP
Integrated Resource Plan
LTAS
Long Term Adaptation Scenarios
NPC
National Planning Commission
EIA
Environmental Impact Assessment
SDA
Sectoral Decarbonization Approach
RCP
Representative Concentration Pathway
Mt
Million tonnes
MtCO2e
Million tonnes of carbon dioxide equivalent
N2O
Nitrous Oxide
NDC
Nationally Determined Contribution
tCO2e
Tonnes of carbon dioxide equivalent
WRI
World Resources Institute
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Key Terms and Definitions1 Climate Change
Climate Variability
Greenhouse Gas (GHG)
Climate Change Impacts
Vulnerability Resilience
Mitigation
Adaptation
Adaptive capacity
1
Climate change refers to a change in the state of the climate that can be identified (e.g., by using statistical tests) by changes in the mean and/or the variability of its properties and that persists for an extended period, typically decades or longer. Climate change may be due to natural internal processes or external forces such as modulations of the solar cycles, volcanic eruptions and persistent anthropogenic changes in the composition of the atmosphere or in land use. Climate variability refers to variations in the mean state and other statistics (such as standard deviations, the occurrence of extremes, etc.) of the climate on all spatial and temporal scales beyond that of individual weather events. Variability may be due to natural internal processes within the climate system (internal variability), or to variations in natural or anthropogenic external forcing (external variability). Greenhouse gases are those gaseous constituents of the atmosphere, both natural and anthropogenic, that absorb and emit radiation at specific wavelengths within the spectrum of terrestrial radiation emitted by the Earth’s surface, the atmosphere itself and by clouds. This property causes the greenhouse effect. Water vapour (H2O), carbon dioxide (CO2), nitrous oxide (N2O), methane (CH4) and ozone (O3) are the primary GHGs in the Earth’s atmosphere. The consequences of realized risks on natural and human systems, where risks result from the interactions of climate-related hazards (including extreme weather and climate events), exposure, and vulnerability. Impacts generally refer to effects on lives; livelihoods; health and well-being; ecosystems and species; economic, social and cultural assets; services (including ecosystem services); and infrastructure. Impacts may be referred to as consequences or outcomes and can be adverse or beneficial. The propensity or predisposition to be adversely affected. Vulnerability encompasses a variety of concepts and elements including sensitivity or susceptibility to harm and lack of capacity to cope and adapt. The capacity of social, economic and environmental systems to cope with a hazardous event or trend or disturbance, responding or reorganizing in ways that maintain their essential function, identity and structure while also maintaining the capacity for adaptation, learning and transformation. Mitigation (of climate change), a human intervention to reduce emissions or enhance the sinks of greenhouse gases. Behaviour change efforts can be planned in ways that mitigate climate change and/or reduce negative consequences of climate change impacts. In human systems, the process of adjustment to actual or expected climate and its effects, in order to moderate harm or exploit beneficial opportunities. In natural systems, the process of adjustment to actual climate and its effects; human intervention may facilitate adjustment to expected climate and its effects. The ability of systems, institutions, humans and other organisms to adjust to potential damage, to take advantage of opportunities, or to respond to consequences.
IPCC, 2014. Fifth Assessment Report of the IPCC, Annex 1: Glossary s.l.: s.n. Viewed 29 July 2019 https://www.ipcc.ch/site/assets/uploads/sites/2/2019/06/SR15_AnnexI_Glossary.pdf
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Introduction Promethium Carbon has been appointed to undertake a Climate Change Impact Assessment as part of the Environmental Impact Assessment process for the Musina-Makhado Energy and Metallurgy Special Economic Zone (EMSEZ, SEZ). The proposed SEZ is located across the Musina and Makhado local municipalities which fall under the Vhembe District Municipality. The Musina- Makhado SEZ objective to create a new heavy industrial hub that forms part of the TransLimpopo Spatial Development Initiative. In accordance with the relevant regulations, an environmental impact assessment process must be completed before project development can proceed. We understand that, in the case of the Musina Makhado SEZ, the current environmental authorisation pertains to the establishment of the SEZ. All activities to be undertaken within the SEZ will be subject to further, individual environmental impact authorisations. Climate change poses major risks to South Africa. The country is located in one of the three regions of the African continent that will most likely suffer significant adverse impacts with predicted warmer and drier summers, wetter and milder winters and more frequent extreme weather events2. The Limpopo province is already experiencing some of these impacts with future predictions indicating increased temperatures and more frequent extreme weather events such as periods of prolonged drought and heat waves 3 . The Province’s water resources, are, and will continue to be significantly impacted by climate change. In addition, there is great social vulnerability within the area as a result of high poverty levels, low levels of education and service delivery backlogs. Climate change impacts could further exacerbate these challenges. The global nature of climate change impact is such that the greenhouse gas emissions from any individual project or source cannot be connected directly to any specific environmental impacts as a consequence of climate change. The analysis presented in this report is presented in the context that, even though the individual GHG emission contribution of a project cannot be directly linked to specific localised climate change impacts, global climate change is significant and can be quantified as such. In other words, the specific greenhouse gas emissions from the SEZ and its eventual tenants cannot be attributed directly to particular climate change effects. Despite this there is a collective responsibility to address the global challenge of climate change and each actor, such as the proposed SEZ, has an individual responsibility to minimise its own negative contribution to climate change.
2 3
Alex Kirby, “Three African Regions at High Risk from Climate Change,” ClimateCentral, 12 June 2019. http://www.climatecentral.org/news/climate-hotspots-imperil-parts-of-africa-17417 Limpopo Provincial Government, Limpopo Provincial Climate Change Response Strategy 2016-2020. 12 June 2019. http://www.ledet.gov.za/wp-content/uploads/2016/11/Limpopo_Climate_Change-Response_Strategy_2016_2020_Final.pdf
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This report covers the climate change impact assessment for the SEZ. Namely, the impact of the SEZ on climate change and the vulnerability of SEZ in terms of climate change. As such an assessment cannot be done without providing context to the potential emissions. As the exact build programme for the SEZ has not been finalised, this report is based on the assumption that the following will form part of the SEZ: • Coal washery • Coke plant • Heat recovery power generation • Thermal power plant • Ferrochrome plant • Ferromanganese plant • Silicon manganese • Vanadium-titanium magnetite • High manganese steel • High vanadium steel plant • Stainless steel Plant • Lime plant • Cement plant • Refractories factory • Sewage treatment plant • Industrial domestic water plant • Light industrial processing zone • Machinery zone • Commercial residential area • Living area • SEZ administration centre • Bonded area
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As the detail designs and related process flows of the envisaged SEZ operations are not yet completed, the emissions associated with these activities cannot be calculated. This assessment considers industry benchmarks and best practice emission intensities required to achieve certain national and international climate change objectives. Ultimately these emissions intensities should form the basis of the environmental approvals for the various operations envisaged in the SEZ. This report also presents emission intensities calculated from data received from the project team and puts it in context with the mentioned intensities. The analysis presented in this report is aligned with the principles of the National Environmental Management Act, 1998 (Act No 107 of 1998), as amended, as it seeks to provide the best possible information to evaluate the project’s environmental sustainability from a climate change perspective. From the outset, the authors of this report want to emphasise the fact that climate change is a global phenomenon, and that South Africa’s domestically focussed environmental laws and regulations have not been yet been amended to take account of international phenomena such as climate change. In this regard the authors of this report, as climate change specialists, have developed, over a period of four years, an appropriate methodology to deal with climate change within the context of domestic environmental legislation. This is defined in detail in Section 4 of this report. However, it is critical to note that given South Africa’s developmental needs and the impacts of climate change on South Africa’s ability to build resilience, a balance must be struck between the immediate social needs of the country, and future environmental impacts. Future environmental impacts, related to issues such as constrained water capacity and biodiversity loss, could have significant socio-economic impacts in terms of increased social climate change vulnerability. It is within the aforementioned context that the SEZ operations have been analysed. The broad terms of reference and scope of work for this specialist climate change assessment include the following: 1. Developing a benchmark greenhouse gas inventory for the SEZ. Due to the fact that detailed information with regards to the operations of each of the activities envisioned for the SEZ is not available, this assessment compiled a benchmark greenhouse gas inventory based on industry benchmarks and current best practice emission intensities. It compares this with high level data provided by the project team. 2. Reviewing the greenhouse gas emissions mitigation options for the project. 3. Conducting an impact assessment of the project: a) Considering its contribution to the South African national emissions inventory, the global greenhouse gas inventory, and the potential impacts of the project on the onset of global anthropogenic climate change; b) Comparing the emissions associated with the value chain of the project against the current South African baseline with consideration of impacts on the future baseline; and
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c) Exploring the potential impacts of global climate change on the risks faced by the project and the project’s broader network. 4. Assessing requirements for greenhouse gas emission management activities for the SEZ’s operations.
1.1 Structure of the Report The following table provides an overview of the NEMA Regulations (2014), Appendix 6 requirements for specialist studies with information on how these requirements have been met in this Climate Change Impact Assessment.
Table 1: Summary of Proposed Projects for SEZ Requirement from Appendix 6 of GN 326 of 7 April 2017 (a) Details of(i) the specialist who prepared the report; and (ii) the expertise of that specialist to compile a specialist report including a curriculum vitae
Chapter Page 12
(b) Declaration that the specialist is independent in a form Page 11 as may be specified by the competent authority (c) Indication of the scope of, and the purpose for which, Chapter 1, Chapter 2 and the report was prepared Chapter 3 (cA) An indication of the quality and age of base data used Chapter 4 for the specialist report (cB) A description of existing impacts on the site, Chapter 3 and 5 cumulative impacts of the proposed development and levels of acceptable change. (d) the Duration, date and season of the site investigation Not applicable and the relevance of the season to the outcome of the change study assessment
to
climate
to
climate
(e) Description of the methodology adopted in preparing Chapter 4 the report or carrying out the specialised process inclusive of equipment and modelling used. (f) details of an assessment of the specific identified Not applicable sensitivity of the site related to the proposed activity or change study activities and its associated structures and infrastructure inclusive of a site plan identifying site alternatives
(g) Identification of any areas to be avoided, including Not applicable to climate buffers change study (h) Map superimposing the activity including the Not applicable associated structures and infrastructure on the change study environmental sensitivities of the site including areas to be avoided, including buffers
to
climate
21
(I) Description of any assumptions made and any Chapter 4 and Chapter 5 uncertainties or gaps in knowledge (j) Description of the findings and potential implications of such Chapter 5 and Chapter 6 findings on the impact ofthe proposed activity, or activities (k) Mitigation measures for inclusion in the EMPr
Chapter 8
(I) Conditions for inclusion in the environmental Chapter 8 authorisation (m) Monitoring requirements for inclusion in the EMPr or Chapter 8 environmental authorisation (n) Reasoned opinionChapter 9 (i) whether the proposed activity, activities or portions thereof should be authorised; (iA) regarding the acceptability of the proposed activity or activities; and (ii)if the opinion is that the proposed activity, activities or portions thereof should be authorised, any avoidance, management and mitigation measures that should be included in the EMPr, and where applicable, the closure plan (o) Description of any consultation process that was undertaken during the course of preparing the specialist report (p) A summary and copies of any comments received during any consultation process and where applicable all responses thereto (q) Any other information requested by the competent authority
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Project Description The following sections provide a context, overview and setting of the proposed Musina-Makhado Energy and Metallurgy SEZ based on information contained in Scoping Report 4 related to the project.
2.1 Regional Project Context The Musina-Makhado SEZ is developed in the following regional context:
4 5
6
•
The Southern African Development Community (SADC) is a Regional Economic Community comprising 16 member states within Southern Africa and promotes sustainable and equitable economic development. The main objectives of SADC are to achieve economic growth, peace and security for the region. South Africa, as a member state aims to promote sustainable development through eradicating poverty by creating employment and sustainable economic growth.
•
The Special Economic Zone (SEZ) Programme has been established by the South African Government as a mechanism to enhance economic development by transforming the local economy into a globally competitive industrial economy. The SEZ programmes are intended to contribute towards strengthening South Africa’s terms of trade through the export of value added commodities, the creation of stronger value chains and provision of much needed jobs in previously disadvantaged regions.
•
The Limpopo Development Plan5 as well as the National Development Plan6 emphasize the need for economic growth which is dependent on provincial resources to help develop competitive industrial areas. It is therefore aimed at the need to utilize the use of locally available resources through various industries for the benefit of the province and the country. The proposed Musina-Makhado SEZ is the single largest proposed SEZ development in the country. It is envisaged that Musina-Makhado SEZ will contribute to the transformation of the governmental agenda in the province in terms of providing regional integration with SADC countries and improving local economic growth.
•
The proposed location for the Musina-Makhado SEZ is central to various coal resources located as well as other minerals such as iron, nickel, manganese, silica and lime stone, all located within a 200km radius. These minerals could provide the inputs to the proposed
Delta BEC, 2019. Musina-Makhado Sepeical Economic Zone Development Scopring Report, Limpopo Province, Revision 01. Limpopo Provincial Government Republic of South Africa: Limpopo Development Plan 2015-2019. Viewed 12 June 2019 http://policyresearch.limpopo.gov.za/bitstream/handle/123456789/1335/LDP%20Draft%20Ver.2.4%20Dec.2 014.pdf?sequence=1 Republic of South Africa: National Development Plan 2030. Viewed 12 June 2019. https://www.gov.za/sites/default/files/Executive%20Summary-NDP%202030%20-%20Our%20future%20%20make%20it%20work.pdf
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projects within the SEZ. The proposed SEZ is located on sections of the N1 motorway and the R525 road with a railway line running along the northwest side. This making it strategically positioned as part of the north south corridor and which could improve trade efficiency by providing a trade route to neighbouring countries. Furthermore, the SEZ could create employment opportunities for the areas which will be presented through various mixed use developments of the industrial park. This could improve economic development for the region and thereby positively contribute to the Southern African Development Countries.
2.2 Project Overview The Musina-Makhado Energy Metallurgical Special Economic Zone (EMSEZ) comprises two sites as designated by the Department of Trade and Industry in July 2016. This report deals specifically with the southern part of the Musina-Makhado SEZ which is located on eight farms (approximately 8,000 hectares) overlapping the border between the Makhado and Musina local municipalities, within the Vhembe District Municipality. The nearest towns are Makhado (located 31 km south) and Musina (located 36 km north) of the proposed SEZ site. This site is situated approximately 34 km from the northern site (Figure 1). The site is a greenfield site and is earmarked for the development of energy and a metallurgical cluster for the production of high-grade steel. The project objective is designed to attract foreign and domestic direct investment to promote industrial development by creating a new heavy industrial hub.
Figure 1: Musina-Makhado Special Economic Zone Proposed Location4. 24
Table 2 indicates the proposed capacity for the different projects comprising the Musina-Makhado SEZ. From this table it is evident that this is a large scale industrial complex which will have varying positive and negative impacts as will be discussed further in this report. Table 2: Summary of Proposed Projects for SEZ7 No. Project
7
Total planned capacity
1
Coal washery
20 000 000 tpa
2
Coke plant
3 000 000 tpa
3
Heat recovery power generation
390 MW
4
Thermal power plant
3300 MW
5
Ferrochrome plant
3000 000 tpa
6
Ferromanganese plant
500 000 tpa
7
Silicon manganese
500 000 tpa
8
Vanadium-titanium magnetite
9
High manganese steel
1000 000 tpa
10
High vanadium steel plant
1000 000 tpa
11
Stainless steel Plant
3000 000 tpa
12
Lime plant
1000 000 tpa
13
Cement plant
2 000 000 tpa
14
Refractories factory
15
Sewage treatment plant
140 000 m3/day
16
Industrial domestic water plant
300 000 m3/day
17
Light industrial processing zone
18
Machinery zone
19
Commercial residential area
20
Living area
21
SEZ administration centre
22
Bonded area
23
Logistics centre
10 000 000 tpa
500 000 tpa
Information not provided
IX engineers, 2019. EMSEZ – Internal Master Planning. Lynwood, Pretoria.
25
The construction phase will cover all leased land and is planned to commence in 2020 pending all required approvals. Table 3 below indicates the timeframes for construction which is anticipated to be complete in 2031. Table 3: Construction phase timeframes7 Project phases Early works and internal bulk infrastructure Phase 1 of plant construction Phase 2 of plant construction Phase 3 of plant construction
Timeframe Start 2020 2022 2026 2029
End 2021 2026 2029 2031
The SEZ comprises various heavy industrial projects which will require a large amount of water for day to day operations. It has been envisaged that the complex will require a feed of 80 million m³ water annually. Figure 2 below indicate the water balance for the proposed operations.
26
Figure 2: EMSEZ Site water balance7. 27
The proposed SEZ envisages to employ 53 800 people. Figure 3 below indicates the employment opportunities for the SEZ.
Figure 3: SEZ total labour figures7.
2.3 Project Setting The proposed project will impact on the surrounding areas in different ways. The section below describes the environmental setting surrounding the proposed SEZ and the various climate change receptors subject to impacts of the SEZ.
The proposed project will be established on eight farm properties across the Makhado and Musina local Municipalities within the Vhembe District Municipality of the Limpopo Province. The current land use of the site is agricultural. The town of Makhado (located 31 km south) and the town of Musina (located 36km north) are the nearest towns to the proposed SEZ.
The proposed SEZ site falls within the Musina Mopane Bushveld which is categorised as least threatened 8 and is regarded as the most diverse Mopaneveld type in South Africa 9 . The land capability of the proposed site is non-arable grazing woodland or wildlife, and wilderness. The soils provide uses for grazing, wildlife management and woodland with limited areas of soil outside the proposed site which are suited to arable agriculture. The historic land cover is indicated in Figure 4 below. 8 9
A least threatened or least concern species are those which has been categorised by the International Union for Conservation of Nature as evaluated but not qualified for any other category. Mucina, L, Ruthford, MC 2006. The Vegetation of South Africa, Lesotho and Swaziland, Strelitzia 19. South African National Biodiversity Institute Pretoria. Viewed 28 May 2019 https://www.sanbi.org/wpcontent/uploads/2018/05/Strelitzia-19.pdf
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Figure 4: Land cover 4.
It is envisaged that the SEZ will require 80 million cubic metres of water per annum, as indicated in Figure 2 above. Table 4 below shows the current and future water balances of the Musina area. The project team has indicated that a large portion of the water will be sourced from the Limpopo River as well as various water bodies in Zimbabwe. For the construction phase, ground water abstraction has been considered along with abstraction of water from the Limpopo River. As the Limpopo Water Management Area forms part of internationally shared water basin between Botswana, Zimbabwe, South Africa and Mozambique, international agreements and obligations will have to be made and met as these countries will be impact by the water demand of the SEZ.
29
Table 4: Current and future water balance of Musina area with interventions 10. Interventions
2015
2020
2025
2030
2035
2040
Water Requirements
Musina area Total Requirements (Musina Town and SEZ)
7.96
31.25
65.52
66.83
70.36
73.36
Sources and Interventions
Zimbabwe to South Africa Water Transfer (Beitbridge Water Supply Scheme and other potential sources)
0
0
30
30
30
30
LEIP Limpopo River abstraction and off-channel storage dam
0
23
23
23
23
23
Reuse of Musina Treated Effluent
0
2
5
7
7
7
Limpopo Alluvial Aquifer
10.4
10.4
10.4
10.4
10.4
10.4
2.44
4.15
2.88
3.57
0.04
- 2.96
Shortfall or surplus
Smaller alternative water reserves are the Nzhelele Dam (50km northeast of Makhado) the Sand River and the Mutamba/Nzhelele River, both perennial rivers that flows mainly in winter and situated 10km north and 20km east of the proposed SEZ respectively. Multiple small wetland are scatted across the eight farms with the proposed SEZ falling within the Limpopo Water Management Areas and the Sand Sub-Water Management Area.
Limpopo has rich biodiversity that forms the basis of a prosperous tourism industry as a result of the Kruger National Park, smaller nature reserves and several luxury private game reserves. It is also home to the Mapungubwe Cultural Landscape, one of South Africa’s eight World Heritage sites. Tourism, along with mining, and agriculture has been identified in the Limpopo Development Plan5 as important sectors to help drive employment and economic growth for the Province. The SEZ site is located within the Vhembe biosphere reserves of which has three biomes, Savanna, grassland and forest. A number of nature reserves and conservation areas have been established in the Vhembe biosphere which aid in conserving the environment and are presented in Figure 5.
10
MMSEZ Progress Report Musina 16 July 2019, RSA/Zimbabwe Water Project, Musina/Makhado MMSEZ Water Supply, National Department of Water and Sanitation, Water Resource Planning, Pretoria, South Africa.
30
Figure 5: Vhembe Biosphere Reserve4 . The proposed SEZ is within an area that is considered a least threatened ecosystem and is surrounded by the Mapungubwe, Soutpansberg and Blouberg Important Bird and Biodiversity areas. The Limpopo Conservation Plan11 categorizes the northern area in which the SEZ site falls as an Ecological Support Area and indicates this area as occurring in a largely natural state that retains significant importance from a landscape connectivity perspective. The Southern areas of the SEZ proposed site is considered a critical biodiversity areas2. Critical biodiversity areas are identified in order to support integrated development planning and sustainable development. Furthermore, they are designed to avoid conflict with existing Integrated Development Plans, Environmental Management Frameworks, and Spatial Development Frameworks in a region by favouring the selection of sites that are least conflicting with other land-uses. Drought and veld fires have been found to be a key biodiversity threats to the area together with limited supply of ground and surface water due to the increasing demand for water with regards to agriculture, mining and domestic use. Coupled with the fact that existing water resource are being negatively impacted due to pollution as a result of pesticides, poor land management and poorly managed sewerage, climate change is expected to exacerbate these treats to biodiversity12.
The proposed SEZ is not located within a formal setting as there is low urban development in the immediate surroundings. The nearest formal towns are Louis Trichardt (Makhado) approximately 40km South and Musina approximately 35km north of the proposed SEZ. The following summary 11
12
Desmet, P. G., Holness, S., Skowno, A. & Egan, V.T. (2013). Limpopo Conservation Plan v.2: Technical Report. Contract Number EDET/2216/2012. Report for Limpopo Department of Economic Development, Environment & Tourism (LEDET) by ECOSOL GIS Vhembe District Municipality, 2016. Vhembe District Municipality Climate Change Vulnerability Assessment Response Plan, s.l.: s.n.
31
of informal settlements which are situated in close proximity to the proposed SEZ site indicated below: •
Matsa - 25km South East
•
Mopane within proposed location - 1km West
•
Mudimeli - 10km South East
•
Makushu - 17km East South East
•
Bonjane - 18km East
•
Numerous farm houses
Figure 6: Percentage of households in informal dwellings in the Vhembe District Municipality12 The percentage of informal households is illustrated in Figure 6 above indicates higher informal dwellings in the Musina and Makhado local municipalities when compared to the Thulamela and Mutale local municipalities. This highlights the vulnerability of the area due to the fact that poorer regions are impacted more by climate change as they do not have the adaptive capacity to withstand significant disruptions brought forth by variable weather such as droughts and floods.
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Climate Change Context 3.1 Global Context Anthropogenic climate change as a global phenomenon is caused by the accumulated greenhouse gas emissions from global emitting sources. The impact thereof on society is increasingly of concern. Recently CO2 levels surpassed 415 parts per million for the first time in recorded history13. Various scenarios have been developed to model climate change impacts for both mitigated (reducing emissions) and unmitigated (business as usual) options. The receiving environment for this project, in the context of climate change, is the global atmosphere. The duration of the impact of the greenhouse gas emissions is considered as effectively permanent as the greenhouse gas emissions produced remain in the atmosphere for an extended period of time. In 2015 the world agreed in the Paris Agreement that the target to limit global warming should be a 2°C increase of average global temperature above the pre-industrial average temperature. The Intergovernmental Panel on Climate Change (IPCC) estimated in the 5th Assessment Report26 that the global limit is to emit a total of 2,900 gigatons of CO2e by 2100, since pre-industrial times. By 2012, a total of 1,890 gigatons of CO2 had already been emitted. This leaves a remaining budget, for the period between 2012 and 2100, of 1,010 gigatons of CO2 before the 2°C limit is breached. The practical implication of having a carbon budget is that this is the maximum amount of emissions that can be emitted. In the context of environmental impact assessments this constitutes a limited resource. If the limit presented by this amount is exceeded, then the planet as whole will suffer irreparable damage with dire consequences to the global society. The Paris Agreement, however, also states that the world should increase ambition and aim for a target of 1.5°C. This is in order to reduce significant and far reaching impacts associated with climate change such as sea rise, desertification, ocean acidification, biodiversity loss and increased frequency and intensity of extreme weather events. The IPCC reported in 2018 an estimate of the remaining carbon budget of 580 gigatons CO2 for a 50% probability of limiting warming to 1.5°C, and 420 gigatons CO2 for a 66% probability (medium confidence)14. The global nature of climate change impacts is such that the greenhouse gas emissions from any individual project or source cannot be connected directly to any specific environmental impacts. The analyses in this report are presented in the context that, even though the individual greenhouse gas emission contribution of a project cannot be directly linked to specific localised climate change impacts, global climate change is nevertheless significant and can be quantified as such. In other
13
14
USA Today, Carbon dioxide levels hit landmark at 415 ppm, highest in human history, viewed 31 May 2019: https://www.usatoday.com/story/news/world/2019/05/13/climate-change-co-2-levels-hit-415-parts-permillion-human-first/1186417001/. IPCC, 2018. IPCC, 2018: Summary for Policymakers of IPCC Special Report on Global Warming of 1.5˚C approved by governments, IPCC, Viewed 31 May 2019: https://www.ipcc.ch/2018/10/08/summary-for-policymakers-of-ipccspecial-report-on-global-warming-of-1-5c-approved-by-governments/
33
words, the specific greenhouse gas emissions from the proposed SEZ cannot be attributed directly to any particular climate change effects. Despite this, there is a collective responsibility to address the global challenge of climate change and each actor, such as the proposed SEZ, has an individual responsibility to minimise its own negative contribution to climate change.
3.2 Local Context The single largest source of GHG emissions in South Africa are coal fired power stations where almost 90% of the country’s electricity comes from. This coal intensive energy system has resulted in the country being the 14th largest GHG emitter in the world and thus a significant contributor to global GHG emissions15. Coal fired power stations not only contribute to climate change but are also at risk from the impacts and consequences of climate change. South African is particularly vulnerable to the effects of climate change with regards to the environment as well and the socio-economic context. The variable nature of climate change in terms of increase frequency and intensity of extreme weather events will be consequential for the South African society. Furthermore, South Africa is a water stressed country with predictions indicating future drying, increased droughts and variable and rainfall. South Africa’s response to climate change South Africa’s National Development Plan 2030 (NDP) is centred on reducing inequality and eliminating poverty by 2030. Climate change impacts and climate change mitigation are highlighted as critical issues in Chapter 5 the NDP. This forms the basis of the following set of goals and action to meet the country’s environmental sustainability and resilience needs have been mentioned16: • Achieving the peak, plateau and decline trajectory (PPD) for GHG emissions; • Entrenching an economy-wide carbon price by 2030; • Implementing zero emission building standards by 2030; and • Achieving absolute reductions in the total volume of waste disposed to landfill each year. South Africa’s climate change response is also set out in the National Climate Change Response White Paper17 which proposed that climate change be addressed through various interventions that build and sustain social, economic and environment resilience by retaining a fair contribution to the global efforts to stabilise GHG concentrations in the atmosphere. South Africa’s Nationally Determined Contribution (NDC) submitted in Paris in 2015 sets out the nation’s emissions trajectory up to 2050. South Africa’s emissions are expected to peak between 2020 and 2025, plateau for approximately a decade and decline in absolute terms thereafter (the ‘peak, plateau and 15 16
17
Global Carbon Atlas, 2017. http://www.globalcarbonatlas.org/en/CO2-emissions Draft, South Africa’s Low Emission Development Strategy 2050, Available at https://www.crediblecarbon.com/wp-content/uploads/2019/07/Draft-South-Africas-Low-EmissionDevelopment-Strategy-2050.pdf Available at https://www.gov.za/sites/default/files/gcis_document/201409/nationalclimatechangeresponsewhitepaper0.pdf
34
decline trajectory’). Overall, the amount of emissions planned to be emitted from 2020 to 2050 within South Africa’s PPD range from 10.6 – 17.0 GtCO2e. South Africa, as a developing nation, requires some allowances to increase its emissions in the short-term, to foster economic growth and steadily transition towards a low carbon economy. However, the South African Government expresses through the White Paper, the Integrated Resource Plan18 that a shift to low-carbon electricity generation options will only be possible in the medium term, and not immediately. South Africa is not limiting itself to specific emissions numbers, but the NDC rather provides a peak, plateau and decline trajectory range from the year 2016 (reference point) to 2050. The country’s lower boundary peak, plateau and decline trajectory pledge is set at 398 Mt CO2e and the upper boundary at 614 Mt CO2e for the years 2025 to 2030. The Climate Change Bill (which is not yet finalised) is expected to make provision for regular updates of this trajectory, through which it can be better placed within the context of the Paris Agreement. However, the issue under consideration is the global shortfall in targets to reach the goal of limiting average temperatures to well below 2°C above pre-industrial levels. In this regard countries such as South Africa must negotiate and determine how to achieve such a target, and how to possibly accelerate efforts to achieve a 1.5°C target through the ratchet mechanism as contained in the Paris Agreement. The ratchet mechanism requires countries to submit new NDCs every five years, outlining how much they intend to reduce emissions. Each submission should be more ambitious than the last. South Africa’s NDC has been assessed as insufficient to meet a 2°C target. A ratcheted South African NDC (which could be categorised as a transitional risk) within the approximate period 2022-2025 could have an impact on the longevity of projects such as the proposed SEZ. In addition to the NDC, the base case of South African draft updated Integrated Resource Plan (IRP)18 incorporates the CO2 emissions constraints as guided by the country’s peak, plateau and decline trajectory. The draft updated IRP applies the moderate decline annual constraints as an instrument to reduce national emissions, which is in line with government policy to reduce greenhouse gas emissions. Government’s policy might change in the future, as per the developments of the Department of Environmental Affairs mitigation system and proposed Climate Change Act. A process is currently being undertaken by the NPC to develop a common vision for the country in 2050. As developing countries will suffer the most from the negative impacts of climate change as a result of a collective failure to limit global emissions, developed countries must take the lead in reducing emissions.
South Africa’s share of this global budget must be seen in the context of the global carbon budget of 1,010 gigatons of CO2 for the 2°C Scenario, as described above. In order to make a reasonable 18
Department of Energy, 2016. Integrated Resource Plan Update Assumptions, Base Case Results and Observations [Online]., Pretoria: Department of Energy. It is noted that the IRP of 2010 was the binding IRP at the time of drafting of this report and that a final updated version of the IRP was published in 2019. However, this still makes provision for coal fired power stations to be built in South Africa.
35
allocation of the country’s fair share to this budget, the global budget was calculated in a per capita basis. The national population figure for South Africa is 58 million people19. If this is taken as a percentage of the global population of 7.7 billion people20, then South Africa’s carbon budget is approximately 7,572 Mt CO2e. The evaluation of the impact of the SEZ on this limited resource will therefore be done by considering its contribution to South Africa consuming its carbon budget. For the 1.5°C Scenario, South Africa’s carbon budget is approximately 4,411 Mt CO2e.
Despite the global and national commitment to limiting global temperature increase to 2°C, the NDCs of all countries combined cover only approximately one third of the emission reductions needed to achieve this goal. Therefore, there will be significant climate change impacts affecting South Africa, and thus the proposed SEZ, regardless of whether the global community implements the NDCs. As a consequence, while the impact of the SEZ on climate change may be small, the impacts of climate change on the SEZ could potentially be large. Risks resulting from climate change impacts may include increasing land-surface temperatures, increasing rainfall variability, decreasing overall rainfall, as well as increasing frequency and intensity of extreme weather events. These risks relate to: •
Decreasing water availability and quality may negatively affect the SEZ’s direct operations as well as the upstream and downstream value chain;
•
Damages to infrastructure which could disrupt operations, transport of goods and lead to increased risk of injury;
•
Labour productivity decrease due to excessive heat exposure;
•
Health of employees which may be compromised due to rising food insecurity and an increased number of casualties as a result of heat effects;
•
Declining air quality may impact on the issuance or conditions of issuance of air quality licences for operations in the SEZ;
•
Disruption to commerce, critical infrastructure and developments, transport systems and traffic by extreme rainfall events and flooding will impact on the SEZ’s ability to operate;
•
Increased number of power outages, water supply and transport disruptions; and
•
Increased risk of infectious, respiratory and skin diseases, water- and food-borne diseases. Pathways for a just transition for the Province of Limpopo
The National Planning Commission (NPC) is currently aiming to build a consensus on a vision and pathway for an equitable and sustainable South Africa in 2050 through the National Development Plan’s, Pathway for a Just Transition. The NPC has agreed that climate change is an urgent and cross cutting issue and will be addressed in all chapters of the NDP. The following 19 20
Stats SA, 2018. Mid-year population estimates 2018. Viewed 31 May 2019 http://www.statssa.gov.za/?p=11341 Worldometers, 2019. Current world population. Viewed 31 May 2019 http://www.worldometers.info/worldpopulation/
36
challenges and issues were identified through the pathway for a just transition workshops conducted by the NPC21; • • •
•
Lack of awareness about climate change and environmental factors; Lack of buy-in from management to enact climate change solutions; Poor planning with regards to future climate change implications. Municipalities do not investigate what the current weather and future climate impacts will be and as a result settlements are situated on climate vulnerable areas such as flood lines; and The need to for strong education and awareness campaign around the impacts of climate change and land-use alongside a capable state.
Climate change management should therefore not be limited to emissions reductions (mitigation) and should focus on adaptation measures as well. Identifying impacts of climate change on the project will therefore be considered in this assessment, which can inform the SEZ’s design, development and closure/rehabilitation strategies to reduce risk exposure and ensure long-term sustainability.
3.3 Observed Trends and Projected Climate Change National overview The impacts of climate change on South Africa have been summarised in the Department of Environmental Affairs’ Long Term Adaptation Scenarios (LTAS) study 22 . However, significant progress has been made in South Africa since the LTAS in terms of the local generation of detailed regional climate futures for the country. The most recent modelling was conducted for South Africa’s Third National Communication23. The past forty years have shown that for South Africa there has been an increase in intensity and frequency of hydro-metrological hazards such as storms, floods, wildfires, droughts and extreme temperatures and it is likely that the frequency of these events will continue to increase in the years to come24. This had impacted 21 million people and claimed the lives 1,692 people in the country25 Furthermore, South Africa is expected to experience high population and urbanisation growth in the next thirty years which emphasises the impacts of an increase in the frequency and intensity of 21 22
23
24
25
The Department of Planning, Monitoring and Evaluation, National Development Plan: Pathways for a Just Transition Limpopo Stakeholder Dialogue Meeting 3 April 2019, Polokwane, Limpopo. DEA, 2013. Long-Term Adaptation Scenarios Flagship Research Programme for South Africa. Climate Trends and Scenarios for South Africa., Pretoria.: Department of Environmental Affairs. DEA, 2017a. South Africa's Third National Communication under the United Nations Framework Convention on Climate Change, Pretoria: Department of Environmental Affairs. UN ESA (United Nations Department of Economic and Social Affairs, Population Division). 2014. World Urbanization Prospects: The 2014 Revision, custom data acquired via website. [Online] Available at: https://esa.un.org/unpd/wup/DataQuery. CRED (Centre for Research on the Epidemiology of Disasters). 2018. EM-DAT: CRED/OFDA International Disaster Database. Brussels: Université Catholique de Louvain. [Online] Available at: http://emdat.be/emdat_db/.
37
extreme weather event on settlements due to a growing exposure to the high socio-economic vulnerability24. With an increase in population expected, more people in these areas are exposed and impacted. Air temperatures in South Africa have increased at least 50% more than the global annual average of 0.65 °C over the last five decades. The IPCC found in its fifth assessment report that it is likely that land temperatures over Africa will rise faster than the global land average, particularly in the more arid regions, and that the rate of increase in minimum temperatures will exceed that of maximum temperatures26. This indicates that in a world of more than 2°C average temperature change, South Africa could experience changes of over 3°C.
Approximate location of South Africa
Figure 7: Projected Southern African temperature change under RCP4.526.
26
IPCC, 2014. Fifth Assessment Report of the IPCC, s.l.: s.n.
38
For the far-future period of 2080-2099, temperature increases of more than 4 °C are likely over the entire South African interior, with increases of more than 6 °C plausible over large parts of the western, central and northern parts. Such increases will also be associated with drastic increases in the number of heat-wave days and very hot days, with potentially devastating impacts on agriculture, water security, biodiversity and human health. From Figure 8 below it is evident that there is a projected decrease in precipitation during the wet season (October to March) towards the year 2100 projected for Southern Africa. Sustained warming and increasing variability in rainfall over the short term (next decade) will have increasingly adverse effects on key sectors of South Africa’s economy in the absence of effective adaptation responses. Early impacts will largely be felt by the poor and vulnerable groups in society. These societal groups are both more exposed and more sensitive to fluctuations in weather patterns and climatic events such as droughts and floods. In addition, poverty and a lack of infrastructure or service provision erodes the adaptive capacity of these communities to climate change, rendering them increasingly vulnerable.
Figure 8: Projected precipitation change for South Africa under different emissions scenarios26 Provincial overview The two most significant climate change projections in the Province are increases in average temperatures and rainfall variability. The Limpopo Province is likely to experience regular droughts and heat intensity, water shortages, and possible diseases spreading related to the chases in climatic conditions which will have adverse effects on the economy, natural resources, infrastructure, human health and community livelihoods. The projected changes as a result of climate change in Limpopo are12: •
Regular droughts and heat intensity;
•
Water shortages;
•
An increase in natural disasters such as floods and fires;
•
Shifts in species and localisation of species; 39
•
Migration of rural populations;
•
Contamination of ecosystems from water and waste pollution; and
•
Increases in communicable and non-communicable diseases in urban and rural areas
3.3.2.1
Temperature
The Limpopo province is highly vulnerable to climate change, with South Africa’s LTAS suggesting that the Limpopo province could face a potential increase in temperatures by as much as 2°C by 2035 with further temperature increase forecasted by as much as 6 °C to 7 °C between 2080 and 21005. Mean temperature ranges between 20 - 22˚C for Makhado and with Musina experiencing hotter conditions with mean temperature ranges of 24-26˚C. The area in which the SEZ is proposed to be located indicates tendencies for drought as well as experiencing elevated temperatures (very hot days) of over 35˚C between 60 and 90 days a year. Figure 9 below shows the projected drought tendencies for the period 1995-2024, relative to 1986-2005 baseline period, under low mitigation scenario (RCP 8.5). A negative value indicates an increase in drought tendencies per 10 years.
SEZ Site
.
.
.
Makhado
.
Thohoyandou
Senwabaranwa Mogwadi
Figure 9: Limpopo drought tendencies for the period 1995-202427.
27
Engelbrecht, F., Le Roux, A., Arnold, K. & Malherbe, J. 2019. Green Book. Detailed projections of future climate change over South Africa. Pretoria: CSIR. Available at: https://pta-gis-2web1.csir.co.za/portal/apps/GBCascade/index.html?appid=b161b2f892194ed5938374fe2192e537.
40
Temperature related climate change impacts include crop loss due to extreme weather conditions and the spread of pests into new areas as temperatures become more favourable. In an area where rural communities depend on cultivating their own crops, changing temperature patterns might cause a decline in rural farming and annual harvests, jeopardising sufficient food levels for these communities. Furthermore, an increase in average temperature levels associated to climate change might have an adverse effect on the SEZ’s labour force as employees work outdoors will therefore be particularly vulnerable to increases in temperature. Consequently, the rising temperatures may pose health hazards, reduce labour productivity, and worsen air quality conditions within SEZ. 3.3.2.2
Rainfall and water
In the case of the proposed SEZ, water is considered from a regional perspective as climate change impacts related to water do not only affect the source of water directly related to the SEZ but also the water areas surrounding the site. It is therefore, extremely important that both surface and ground water studies be conducted to delineated availability, capacity and future balances as a result of the water demand for the SEZ as well as the water demand of a growing population within the Musina and Makhado municipalities. Rainfall averages 588mm per annum in Makhado and decreases moving north towards Musina which has an average of 426 mm per annum. For both these areas the majority of the rainfall falls in the summer months of October through to January. The proposed SEZ site is located within a low to medium flooding hazard with areas approximately 25km South and South East of the proposed SEZ site being indicated as high to very high flood hazards. Figure 10 below shows the flood Hazard index of the different quinary catchments present or intersecting with the municipality. The flood hazard index is based on the catchment characteristics and design rainfall, average at the quinary catchment level.
41
SEZ Site
. . .
.
Makhado
.
Thohoyandou Malamulele
.
Senwabaranwa Mogwadi
.
Giyani
Modjadjiskloof
Figure 10: Flood Hazard index27. Rainfall projections for the Limpopo Province show levels of uncertainty however, evidence suggests decreases in annual rainfall22. The combination of significantly increased temperatures and lessened rainfall will contribute to an increase in evaporation rates, further implying a drier future despite the possibility of periodic heavy rainfall events. The current and projected climatic variability will greatly impact on Limpopo’s water supply and quality provision, which could in future constrain the province’s economic growth. This is specifically relevant in the provincial context of the proposed SEZ as the Limpopo province is already vulnerable to droughts and variable rainfall patterns. Water intensive sectors, such as energy and metallurgical industries that will be located in the SEZ could face major operational challenges. Municipal overview The proposed SEZ falls on the boarder of the Musina and Makhado Local Municipality, located in the Vhembe District Municipality. Vhembe District Municipality comprises four local municipalities namely; • Makhado Local Municipality (population 516,031); • Musina Local Municipality (population 68,359) • Thulamela Local Municipality (population 618,462); and • Mutale Local Municipality (population 91,870)
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District has a total population of approximately 1,294,72228. It has a high unemployment rate of 24.9% with 50.8% not economically active and only 21.26% of the population having a matric certificate 12. During 2016 the Vhembe District Municipality developed a Climate Change Vulnerability Assessment and Response Plan to address the threats posed by climate change on sustainable development. Key climate change vulnerability indicators were identified as part of the District’s climate change assessment. The relevant indicators within the context of the project location and scope are summarised in the following table: Table 5: Vhembe District Municipality key climate change vulnerability indicators12. Theme
Indicator Title
Agriculture
Biodiversity and Environment Human Health
Human Settlements, Infrastructure and Disaster Management
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Exposure
Sensitivity
Reduced food security Change in grain (Maize, wheat & barley) production Loss of Grasslands
Yes Yes
High High
Adaptive Capacity Medium Low
Yes
High
Medium
Health impacts from increased storm events Increased heat stress Increased vector borne diseases from spread of mosquitoes, ticks, sand flies, and blackflies Increased water borne and communicable diseases (typhoid fever, cholera & hepatitis) Increased malnutrition and hunger as a result of food insecurity Increased air pollution Increased Occupational health problems Increased isolation of rural communities Increased migration to urban and peri-urban areas. Note that climate change impacts in other areas in South Africa, as well as its neighbouring
Yes
High
Low
Yes Yes
High High
Low Medium
Yes
High
Low
Yes
High
Medium
Yes Yes
Low High
Low
Yes
High
Medium
Yes
High
Low
Stats SA, 2018. Popoulation Limpopo, 2019. Viewed 3 June 2019 Available at: http://www.statssa.gov.za/?page_id=964
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Water
countries can cause migration to SDM Less water available for irrigation and drinking Decreased water quality in ecosystem due to increased concentrations of effluent and salt concentrations
Yes
High
Low
Yes
High
Low
Additionally, Agriculture, Forestry and Fisheries (AFF) contributes 13.76% to total employment in the Makhado municipality and 0.7% to the national AFF Gross Value Add (GVA). Musina AFF contributes significantly more jobs (36%) to the area, and yet contributes less (0.52%) to the national AFF GVA. As indicated in the above table, the Vhembe District municipality has a low adaptive capacity with regards to impacts of climate change on agriculture. This threatens the sustainable development of the district which relies on AFF for employment. Furthermore, the South African online planning tool, the Green Book, provides quantitative scientific evidence on the likely impacts that climate change and urbanisation will have on South Africa’s cities and towns. The Green Book has quantitatively rated all South African municipalities using multi-dimensional vulnerabilities such as socio-economic, economic, physical and environmental. Musina and Makhado are rated 195 and 168 respectively out of 213 municipalities (higher rating indicates higher vulnerability) in South Africa in terms of environmental vulnerability, an indicator representing the conflict between preserving the natural environment and accommodating the growth pressures associated with population growth, urbanisation and economic development. This again emphasizes the vulnerability of the municipalities to the disrupting effects of climate change and further highlights the need for careful consideration of the climate change implications that constriction of large industries could impose on the municipalities’ resource dependency.
3.4 Other Potential Climate Change Dimensions Relevant to the SEZ Other potential climate change risks are those that relate to climate change but cannot be classified as physical or regulatory risks. These risks can include: • Reputational risk, especially concerning negative perceptions of the general public or investors; •
Changes in consumer behaviour relating to customer preferences for products/services;
•
Induced changes in human and cultural environments (for example, migration and cultural changes);
•
Fluctuating socio-economic conditions;
•
Increasing humanitarian demands, as climate change impacts are experienced. 44
South Africa, and the Limpopo Province, has an economically divided society due to a number of socio-economic disparities. As a result, its population is characterized by a vulnerable majority. The vulnerable majority is more exposed to climate change impacts and may pose risks to large industrial developments such as the SEZ, either through migration of workforces or increased humanitarian demands.
Methodology 4.1 Impacts of the Project on Climate Change The following subsections outline the methodology used to assess the impacts the MusinaMakhado SEZ development will have on greenhouse gas emissions. The results of the carbon footprint calculations and the assessment of its environmental impacts are presented in section 6 of this report. The methodology used to assess the impact of the project on climate change was developed in the context that data, such as plant/process design, fuel/energy consumption and construction plans, could not be provided by the client for the various planned activities within the SEZ. What little data was provided could not be reliably corroborated with any supporting evidence. Greenhouse gas emissions estimation methodology The emissions calculated in this report consider the emissions from activities envisioned as part of the SEZ. An umbrella approach was followed for the SEZ which considered the emissions of the SEZ in its entirety. This report assumed that an Environmental Impact Assessment (EIA) and related climate change impact assessment, including establishing a greenhouse gas inventory, will be completed for each of the proposed activities within the SEZ. As the designs for the various activities and related plants envisaged for the SEZ, as listed in Table 2 above, has not yet been finalised, the emissions for each of these plants cannot yet be calculated. Therefore, this assessment has determined emission intensities for the various activities envisioned within the SEZ (based on available information), required to achieve national and international climate change objectives. These intensities should serve as suggested benchmarks to guide and inform the environmental authorisation processes related to each of the activities to take place within the SEZ. This methodological approach is illustrated in the following figure:
45
Indicative emissions calculated for entire Special Economic Zones
Emission intensities guidelines to be used for further environmental authorisations
Musina-Makhado Special Economic Zone
Individual EIAs
Industry intensity benchmarks Individual EIAs
Best practice intensities
Individual EIAs
Figure 11: Proposed Methodology boundary and input
The calculation of the various emission intensities was a 2-step process: Step 1:
Step 2:
Historic and current best practice emission intensities were determined. These emissions were calculated making use of industry benchmarks and carbon emission intensities published in the “GHG Emissions Intensity Benchmarks for South Africa’s Carbon Tax” prepared by Ecofys for National Treasury. This formed the starting point of the assessment. The second step was to contextualise the emission intensities in relation to national and international targets and commitments. In this regard, South Africa’s Nationally Determined Contribution (NDC) to the Paris Agreement was considered.. However, as the Paris Agreement has called for more progressive commitments were possible, the 2018 IPCC 1.5°C Special Report was used as a point of reference as well. The NDC allows for a Peak Plateau and Decline (PPD) trajectory for South Africa, whereas the IPCC 1.5°C Report goes further and proposes that the world as a whole should have net-zero emissions by 2050. It was assumed that the various activities envisioned as part of the SEZ will be operational by 2030. The plants associated with the various activities in the SEZ will be operational under intense emission reduction pressure, both locally and globally. From a global perspective, in order to achieve a 1.5°C temperature target, the emissions from the plants should reach zero over their expected lifetime. Locally, South Africa’s NDC commitments requires significant emission reductions from 2035 onwards. The intensity methodology thus assumes that the intensity the plant will be built with would represent its emission intensity for at least the first ten years of its operating 46
life. In this respect, individual plants/activities should meet the suggested 2030 emission intensities as part of their respective environmental authorisation processes. This analysis used an internationally accepted methodology to estimate what the emission intensities by 2030 should be, for a 2°C target, as developed by the Science Based Target Initiative (SBTi)29. Detailed information is not yet available for the construction phase for each of the individual plants. As mentioned, it is assumed that an EIA and related climate change impact assessment will be completed for each of the applicable activities within the SEZ. During such an assessment, it is assumed that the required level of detailed data will be made available which can be used to calculate the emissions associated with the construction and decommissioning phases of each of the activities. Due to the nature of the various activities envisioned for the SEZ, these plants will have high process emissions during the operational phases. Compared to the process emissions, it is expected that the construction and decommissioning phase emissions of the plants will be insignificant. Nevertheless, it is important that the impacts of climate change are considered in the decommissioning and rehabilitation plans within each of the separate EIAs. The South African Greenhouse Gas Reporting Technical Guideline prescribes that direct emissions be considered for mandatory greenhouse gas reporting. The intensity methodology applied to this study considers the various direct emissions from the various planned activities within the SEZ. As such this methodology meets South Africa’s Greenhouse Gas Reporting regulations. Following the above, the calculation of the emissions were done as indicated in sections 4.1.1.1 and 4.1.1.2 below. 4.1.1.1
Current industry emission intensity benchmarks
The intensities presented in Table 6 below are presented in tonnes of carbon dioxide equivalent (tonne CO2e) per tonne of output product. The intensities include both Scope 1 and 2 emissions. The benchmarks represent the global industrial average emission intensity for the identified industries.
29
https://sciencebasedtargets.org The SBTi is one of the mechanisms that can assist in meeting the Paris Agreement outcomes. Its agenda is to align the emission reduction targets to scientifically established global carbon budgets. The initiative is motivated by the fact that, to date, global actions and the NDC commitments from states are not sufficient to meet the global objective of limiting temperature increases to 2°C. The SBTi states that emission reduction targets are ‘sciencebased’ if they are in line with the level of decarbonisation required to keep global temperature increase below 2°C compared to pre-industrial temperatures, as described in the Fifth Assessment Report of the IPCC.
47
Table 6: Emission intensity benchmarks used Plant
Value
Unit
Reference
0.3 - 0.5
t CO2e/t product
GHG Emissions Intensity Benchmarks for SA Carbon Tax - Ecofys
Ferrochromium plant*
4.49
t CO2e/t product
GHG Emissions Intensity Benchmarks for SA Carbon Tax - Ecofys
Ferromanganese plant*
4.49
t CO2e/t product
GHG Emissions Intensity Benchmarks for SA Carbon Tax - Ecofys
Pig iron plant
1.4-1.7
t CO2e/t product
GHG Emissions Intensity Benchmarks for SA Carbon Tax - Ecofys
Carbon steel plant
0.6 - 0.7
t CO2e/t product
GHG Emissions Intensity Benchmarks for SA Carbon Tax - Ecofys
Stainless steel plant
1.11
t CO2e/t product Energy Use and Carbon Emissions in the Steel Sector in Key Developing Countries
Lime plant
1.092
t CO2e/t product
A competitive and efficient lime industry, cornerstone for a sustainable Europe (2014)
Cement plant
1.0
tCO2e/t clinker
Benchmarking study conducted by Promethium Carbon
Silicon- manganese plant
6.9
t CO2e/t product
LCA - Environmental profile of manganese alloys: International Manganese Institute
Coke plant
Sewage treatment plant
0.000708
t CO2e/t water
DEFRA 2018
Water treatment plant
0.000708
t CO2e/t water
DEFRA 2018
* These intensities were adjusted to align with an energy intensity of 3.5MWh/tonne. This value was obtained from consultations with an international ferroalloy expert.
4.1.1.2
Emission intensities for a 2°C target by 2030
The Sectoral Decarbonisation Approach (SDA) method of the Science Based Target Initiative (SBTi) is based upon trajectories for specific sectors. The SDA method projects that the global production of crude steel will increase to 2.295 Mt by 2050. This is an increase of 55% on 2010 production levels of 1.482Mt. Despite this increase in demand, the SDA requires that a reduction of 31% in total emissions from the Iron and Steel sector is required in order to meet a 2°C target (Science Based Targets Initiative, 2015). The SBTi has published a tool for calculating targets based on the SDA approach as well as the absolute contraction approach. This tool has been used to calculate the emissions intensity the plants should have in 2030 to align with the 2°C target trajectories. In the calculations it was assumed that the benchmark intensities used in the carbon footprint would be applicable to the plant in 2020. It is also assumed that the production output capacity remains the same going
48
forward. Where there was no applicable SDA sector then the Absolute Contraction Method was used. The resulting intensities can be seen in the table below. The target trajectories for the pig iron and carbon steel plants can be seen in the figure below. The pig iron and carbon steel plants were combined to align with the SDA sector definition. Table 7: Emission intensities required to achieve the Paris Agreement 2°C goal Plant Coke Plant Ferrochrome plant Ferromanganese plant Silicon-manganese plant Carbon steel plant Stainless steel plant Lime plant Cement plant Sewage treatment plant Water treatment plant
2°C target intensities for 2030 0.21 tCO2e/tonne product 3.37 tCO2e/tonne product 3.37 tCO2e/tonne product 5.18 tCO2e/tonne product 0.37 tCO2e/tonne product 0.78 tCO2e/tonne product 0.87 tCO2e/tonne product 0.80 tCO2e/tonne clinker 0.0005 tCO2e/tonne water
0.0005 tCO2e/tonne water
It is important to note that these intensities are not the current industry intensities, they are the maximum allowable intensities to align with the 2°C target trajectories according to the Science Based Target Initiative. It is also noted that it is beyond the scope of this Climate Change Impact Assessment to determine how the various industries in the proposed SEZ will achieve the above proposed target emission intensities. Environmental impacts of greenhouse gas emissions The environmental impact assessment reporting requirements listed below set out the criteria to describe and assess local environmental impact. However, climate change is a global phenomenon thus the criteria are only partially applicable to the assessment of the impacts of greenhouse gas emissions on climate change. Despite this, these criteria are currently the available tool for a climate change impact analysis and will therefore be used in this assessment. Table 8: Environmental impact assessment criteria Nature
A description of what causes the effect, what will be affected and how it will be affected. In the case of climate change assessments, the nature of the impact is the contribution of the project to global anthropogenic climate change.
Extent (E)
An indication of whether the impact will be local (limited to the immediate area or site of development) or regional, and a value between 1 and 5 will be assigned as appropriate (with 1 being low and 5 being high). In the case of climate change assessments, the extent is always global, and thus a 5 is allocated to all projects that contribute to global anthropogenic climate change. 49
Duration (D)
An indication of the lifetime of the impact quantified on a scale from 1-5. Impacts with durations that are; very short (0–1 years) are assigned a score of 1, short (2-5 years) are assigned a score of 2, medium-term (5–15 years) are assigned a score of 3, long term (> 15 years) are assigned a score of 4 and permanent are assigned a score of 5. In the case of climate change assessments, the duration is always long term, and thus a 5 is allocated to all projects that contribute to global anthropogenic climate change.
Magnitude (M)
An indication of the consequences of the effect quantified on a scale from 0-5. A score of 0 implies the impact is negligible, 1 is minor, 2 is low and will cause a slight impact, 3 is moderate, 4 is high with sizable changes, and 5 is very high resulting drastic changes. This is the context within which the environmental impact assessment reporting requirements were developed to describe and assess environmental impacts. However greenhouse gas emissions that have a global impact have yet to be described appropriately within South Africa’s legal environment. For this reason, a materiality threshold was defined. South Africa’s carbon budget is described in 3.2.2 above. In an attempt to align the reality of climate change impacts with the requirements of NEMA, the following impact ratings (and scores) have been identified as a means of benchmarking greenhouse gas inventories, over the lifetime of the specific activity, related to emissions that occur within the boundaries of South Africa. Table 9: Greenhouse gas emissions impact rating
South Africa's carbon budget based on proportion of local population (2°C target) Low impact by project – emissions up to: Medium: impact by project – emissions up to: High: impact by project – emissions up to: Very High: impact by project – emissions in excess of:
Probability (P)
Greenhouse gas inventory 7,572 MtCO2e
% of South African carbon budget
Score
10,000 tCO2e
0.00013%
1
1,000,000 tCO2e
0.013%
2
10,000,000 tCO2e
0.13%
4
>10,000,000 tCO2e
>0.13%
5
The magnitude of a project is considered very high (5) if the emissions are in excess of 0.13% of the South African carbon budget and low (1) if they fall below 0.00013% of the South African carbon budget. An indication of the likelihood of the impact actually occurring estimated on a scale of 1–5. A score of 1 implies that the impact is very improbable, 2 are improbable, 3 are probable, 4 are highly probable and 5 are definite with the impact occurring regardless of any prevention measures. The IPCC has reported that it is 95 percent certain that man-made emissions are the main cause of current observed climate change. Thus, a value of 5 is allocated to all projects that contribute to global anthropogenic climate change.
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Significance (S)
The significance points are calculated as: S = (E + D + M) x P. A weighting based on a synthesis of the characteristics described above and can be assessed as low (< 30 points), medium (30-60 points) or high (> 60 points).
Carbon Capture and Storage (CCS) technologies remove CO2 emissions from the emission streams of processes and sequester them in the ground. This is achieved in such a manner that the CO2 is not released back into the atmosphere. According to Sanedi (2017)30, CCS could have a great potential in assisting South Africa meets its committed Peak, Plateau and Decline scenario. However, there are currently still significant barriers to economical deployment of CCS in South Africa. These are the following: • A lack of legislative and regulatory support exists within South Africa’s legal frameworks to encourage investment in and development of CCS technology in South Africa. • Current predictions of existing CCS technology and research from around the world indicates that CCS will only become economically viable no sooner than 2030 and might take as long as 2040 or even 2050, to become economically viable. • Carbon pricing plays a significant role in the economic viability of CCS. Current carbon pricing in national and international markets is too low to make CCS look like a viable alternative. Based on the above, we recognise that the implementation of CCS would currently be a challenging endeavour for any project. We also recognise that the challenges mentioned above will have an impact on the economic viability of the MMSEZ. The IPCC’s 6th Assessment Report from Working Group I provides further context for the need of CCS. This report highlights the extent of observed and projected climate change based on several possible future scenarios. Even under a very good mitigation scenario, best case scenario estimates still show an average temperature increase of 1.5°C in the near term (2021-2040) and 1.4 °C in the long term (2081-2100). This very good mitigation scenario would require a steep decline in global CO2 emissions with immediate effect, with global emissions being 50% of current levels by 2030 and a carbon neutral world by 2050. Such a scenario would require the implementation of CCS technologies on high CO2 emission sources, such as coal fired power stations. Furthermore, South Africa would need to aim for this approach to meet its commitments in terms of the Paris Agreement.
4.2 Impacts of Climate Change on the Project The impacts of climate change on the project is assessed for two reasons. Firstly, the analysis is intended to establish whether or not the project has sufficiently considered the effects of climate change in terms of its design. This is important, as the EIA considers the impact of the project on
30
Sanedi (2017). Business Case for the Continued Investigation of Carbon Capture and Storage in South Africa.
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the environment, but if the environment is due to change as a result of climate change during the life of the project, then this should be considered in the EIA. Secondly, the impact of climate change on the project is considered as it relates to the guidance provided by the judgement in the Thabametsi Case31. The potential impact of climate change on the SEZ is analysed through a climate change vulnerability assessment related to both the construction and operational phases. Vulnerability relates to the degree to which a system is susceptible to, and unable to cope with, adverse effects of climate change, including climate variability and extremes weather events. Vulnerability is a function of a number of variables, including the character, magnitude and rate of climate change, the variation to which a system is exposed, its sensitivity and its adaptive capacity32. The assessment considered risks from the perspective of climate change impacts on temperature, water, biodiversity, transitional risks and the social context and how this influences the SEZ’s core operations, value chain and the broader network. This approach is in line with guidance from the International Council on Mining and Metals. • The core operations include activities taking place within the operational functioning of the SEZ. • The value chain includes the upstream goods and services, as well as the downstream use of product. • The social context of the proposed SEZ in terms of the climate vulnerability; and • The natural environment with regards to climate impacts. By identifying the levels of exposure, sensitivity, potential physical and transitional risks and adaptive capacity, it can be assessed whether and to what extent the SEZ’s core operations, value chain and broader social and natural environment are vulnerable to climate change. The following figure provides a schematic overview of the approach to the vulnerability assessment.
31 32
High Court of South Africa judgement on Thabametsi power project Available at https://cer.org.za/wpcontent/uploads/2017/03/Judgment-Earthlife-Thabametsi-Final-06-03-2017.pdf Parry, M., Canziani, O. & (eds.), e. a., 2007. Climate Change 2007: Impacts, Adaptation and Vulnerability, Contribution of Working Group II to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, s.l.: s.n.
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Current and future climate variability and change
Exposure
Sensitivity
Adaptive Capacity
Potential risks
Vulnerability
Core Operations
Value Chain Up/down stream
Natural Environment
Social Environment
Figure 12: Vulnerability assessment process The vulnerability assessment considers the core operations of the proposed project, the project’s value chain as well as the social and natural environment which could impact the project or be impacted on by the project. Exposure refers to what extent a system is being subjected to climate factors (e.g. temperature, precipitation). To which degree a system or group is positively or negatively affected by climate change exposure is defined by sensitivity. Only factors that directly impact the climate (change) are considered sensitivities. Risks are identified based in the climatic parameters identified in the describing the receiving environment, and how exposed and sensitive the project is in relations to these climatic changes. Adaptive capacity refers to “a set of factors which determine the capacity of a system to generate and implement adaptation measures” (GIZ 2014, p. 24) which is relevant to the project’s core operations. Once all of these elements have been assessed, the vulnerability of a specific project can be defined. Vulnerability is indicated as high, medium or low, as defined by the following table.
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Table 10: Musina Makhado SEZ Climate Change Risk and Vulnerability Analysis Components Risk analysis component High risk
Medium Risk
Low Risk
Legend and definition High risk implies a high likelihood of the identified MM SEZ risk being worsened / exacerbated under a high or a low mitigation scenario. It also suggests a high impact of the risk under a high or a low mitigation scenario. For example, a shutdown of the operations. Medium risk implies a likelihood of the identified MM SEZ risk being continued under a high or a low mitigation scenario which is still material to the SEZ’s core operations, value chain and the broader community. Low risk implies a lower likelihood of the identified MM SEZ risk being worsened / exacerbated under a high or a low mitigation scenario. It also suggests a lower impact of the risk under a high or a low mitigation scenario to the SEZ.
Climate change-related risks were divided into two major categories, namely physical risks and transitional risks. This follows the Task Force on Climate-Related Financial Disclosures’ (TCFD) new, only recently published, direction around standardised assessment and reporting of climate change risks. The TCFD defines physical and transitional risks as follows: •
Physical risks: Physical climate change risks can be event driven (acute) or can be longerterm shifts (chronic) in climate patterns. Physical risks may have financial implications for the proposed SEZ, such as interruption of operations, direct damage to assets and indirect impacts from supply chain disruption.
•
Transition risks: Transitioning to a lower-carbon economy may entail extensive policy, legal, technology, and market changes to address mitigation and adaptation requirements related to climate change. Depending on the nature, speed, and focus of these changes, transition risks may pose varying levels of financial and reputational risk for the proposed SEZ.
The risks are classified as either low or high depending on the emissions scenario. Physical risks are higher and regulatory risks are lower under the climate change scenario related Concentration Pathway (RCP) 8.6 scenario (unmitigated emissions scenario), as this scenario is expected to increase global temperatures by 6 C which would for example increase the risk of heat stress. Typically, physical risks are lower and regulatory risks are higher under the climate change scenario related to the Nationally Determined Contribution or a Representative Concentration Pathway (RCP) 2.6 scenario (mitigated emissions scenario), as this scenario aims to keep temperatures at 2 C or below. The mitigated emissions scenario is supported by the Paris Agreement and will be achieved as countries set ambitious Nationally Determined Contributions (NDCs). As country’s work towards their NDCs, additional regulations may be put in place to limit emissions from fossil fuel intensive industries or encourage renewable energy development. 54
Impact of Project on Climate Change The impact assessment of the project on climate change was determined in the context that data, such as plant/process design, fuel/energy consumption and construction plans, could not be provided by the client for the various planned activities within the SEZ. What little data was provided could not be reliably corroborated with any supporting evidence.
5.1 Quantification of the Project’s Greenhouse Gas Emissions A greenhouse gas emission indicator report was provided by the client and the emissions contained therein are summarised in the table below. The list of facilities and projects provided in this report is as per information received to date as well as the latest version of the SEZ masterplan. Table 11: Emissions provided in the Greenhouse Gas Emission Indicator Report Project
Total indicative planned capacity
Total emissions
Intensity Calculated from data provided
Coal washery
20 000 000 tpa
No data provided
-
Coke plant
3 000 000 tpa
No data provided
-
Heat recovery power generation
390 MW
No data provided
-
Thermal power plant
3300 MW
19.62 MtCO2/yr
0.85 tCO2e/MWh
Ferrochrome plant
3000 000 tpa
3.96 MtCO2/yr
1.32 tCO2e/t
Ferromanganese plant
500 000 tpa
1 MtCO2/yr
1.0 tCO2e/t
Silicon manganese
500 000 tpa
0.66 MtCO2/yr
1.32 tCO2e/t
10 000 000 tpa
5.28 MtCO2/yr
0.53 tCO2e/t
High manganese steel
1000 000 tpa
No data provided
-
High vanadium steel plant
1000 000 tpa
No data provided
-
Stainless steel Plant
3000 000 tpa
No data provided
-
Lime plant
1000 000 tpa
1.25 MtCO2/yr
0.25 tCO2e/t
Cement plant
2 000 000 tpa
0.51 MtCO2/yr
0.26 tCO2e/t
500 000 tpa
No data provided
-
Sewage treatment plant
140 000 m3/day
No data provided
-
Industrial domestic water plant
300 000 m3/day
No data provided
-
Vanadium-titanium magnetite
Refractories factory
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Light industrial processing zone
No data provided
No data provided
-
Machinery zone
No data provided
No data provided
-
Commercial residential area
No data provided
No data provided
-
Living area
No data provided
No data provided
-
SEZ administration centre
No data provided
No data provided
-
Bonded area
No data provided
No data provided
-
Logistics centre
No data provided
No data provided
-
Areas for which no data was provided are considered to not have material emissions and are therefore not taken into consideration for the rest of this analysis. The greenhouse gas emissions of the envisioned activities in the SEZ, if the plants are built to have emission intensities as provided in Table 5 above, have been calculated and are shown in Table 12 below. The calculation is based on: Emissions (tCO2e) = Production (tons product) x emission factor (tCO2e/ton product) The calculation was done for emission factors based on current industry benchmarks. Note that the intensities include both scope 1 and scope 2 (energy indirect) emissions. As it is assumed that the electricity produced by the proposed coal fired power station is consumed on the site, reporting of the emissions from the plant would result in double counting in this specific table. The emissions from the coal fired power plant is therefore not reported in Table 12 below. Table 12: Annual project emissions Plant Coal Washery Coke Plant Heat Recovery power generation Coal-fired power plant Ferrochrome plant Ferromanganese plant Silicon-manganese plant Carbon Steel Plant Stainless Steel Plant Lime Plant Cement Plant Sewage Treatment Plant Water Treatment Plant Total SEZ
2010 historic intensities used
0.3 tCO2e/t product
4.49 tCO2e/t product 4.49 tCO2e/t product 6.9 tCO2e/t product 0.6 tCO2e/t product 1.11 tCO2e/t product 1.092 tCO2e/t product 1.0 tCO2e/t product 0.000708 tCO2e/t water 0.000708 tCO2e/t water
Emissions based on 2010 historic intensities 900 ktCO2e/y * * 13.5 MtCO2e/y 2.2 MtCO2e/y 3.5 MtCO2e/y 7.2 MtCO2e/y 3.3 MtCO2e/y 1.1 MtCO2e/y 2 MtCO2e/y 99 tCO2e/y 212 tCO2e/y 33.7 MtCO2e/y
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*Note: See comment above the table - It was assumed that all electricity consumed by the plants in the industrial complex was produced by the onsite power plant. The Scope 2 emissions included in the calculations therefore relate to the electricity produced at this power plant. The emissions from the power plant are thus excluded to avoid double counting.
Millions
Emissions (MtCO2e)
The proposed Musina-Makhado SEZ development is expected to generate approximately 1 billion tonnes of carbon dioxide equivalent of direct and energy indirect emissions over the lifetime of the project. The largest contributors to these emissions are the ferrochrome, lime and carbon steel plants. A breakdown of these emissions is illustrated in the figure below. 450 400 350 300 250 200 150 100 50 -
Project Type
Figure 13: Emissions per project type for the 30 year life of the project There are no emission intensities allocated for the waste generated by these activities. The majority of the waste that would be generated by these activities would not be degradable and would not release GHG emissions. Furthermore, the general waste generated by the workforce employed at the proposed SEZ would have been generated anyway by said workforce, even if the SEZ would not be declared. However, it could be argued that a portion of the waste generated should still be allocated to the SEZ. In such an event, the per capita emissions generated from solid waste management, as calculated using the National Greenhouse Gas Inventory33 and the population reported by Stats SA34, could be allocated to the workforce. The annual emissions from solid waste management would then amount to 40 600 tCO2e/annum. This is negligible relative to the scale of the other emission sources within the proposed SEZ. The emissions associated with the land use change/degradation of the land and the subsequent release of sequestered carbon will be approximately 401 000 tCO2e. This was calculated using the online Carbon Sinks Atlas Tool 35 provided by the Department of Environment Forestry and Department of Environmental Affairs (2015). South Africa’s Greenhouse Gas Inventory Report, 2000 – 2015. [Online] http://www.statssa.gov.za/?p=12362. [Accessed on 03/12/2020] 35 [Online] https://ccis.environment.gov.za/carbon-sinks/#/explore-data. [Accessed on 03/12/2020] 33 34
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Fisheries. This amounts to 0.04% of the lifetime emissions of the proposed SEZ and is considered to be negligible. Furthermore, the ecosystems in the proposed SEZ are well established ecosystems that have reached steady-state (i.e. rate of growth is equal to the rate of decay). Thus, there is limited potential for this land to act as an even larger carbon sink and store significantly more levels of carbon than it currently is.
5.2 Impacts on Greenhouse Gas Inventories The impacts of the Musina-Makhado project’s emissions must be considered within the context of both national and international greenhouse gas reduction plans. This will provide for a more holistic understanding of these impacts.
Impact ratings of greenhouse gas emissions have been identified to benchmark greenhouse gas inventories, as described in Table 8 above. These ratings apply to emissions that occur with the boundary of South Africa and are as follows: • Low: Emissions up to 10 thousand tCO2e/yr, or 0.00013% of South Africa’s carbon budget • Medium: Emissions up to 1 million tCO2e/yr, or 0.013% of South Africa’s carbon budget • High: Emissions up to 10 million tCO2e/yr, or 0.13% of South Africa’s carbon budget • Very High: Emissions of more than 10 million tCO2e/yr, or 0.13% of South Africa’s carbon budget In the light of this classification, the Musina-Makhado emissions of more than 10 million tons per year has a VERY HIGH impact. The Musina-Makhado SEZ’s calculated emissions inventory in relation to South Africa’s remaining portion of the global carbon budget as per Table 8, is presented in Table 13 blow: Table 13: The Musina-Makhado SEZ development's emissions relative to South Africa's carbon budget Emissions South Africa’s carbon budget Scope 1 and 2 emissions of the project activities using 2020 industry benchmark intensities over the life of the project Scope 1 and 2 emissions of the project emissions using 2°C target intensities for 2030 over the life of the project
2°C Target 7,512 Mt CO2e 1,010 MtCO2e - equivalent to 13-14% of SA’s carbon budget
1.5°C Target 4,411 Mt CO2e 1,010 MtCO2e - equivalent to 23-24% of SA’s carbon budget
728 MtCO2e - equivalent to 10% of SA’s carbon budget
728 MtCO2e - equivalent to 16% of SA’s carbon budget
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The impact of the Musina-Makhado project’s greenhouse gas inventory is considered to be VERY HIGH due to the total emissions from the project being between 10% and 14% of South Africa’s carbon budget, considering the 2°C target carbon budget. This impact assessment should also be considered in the context of the local policy environment. South Africa submitted their Nationally Determined Contribution (NDC) in response to the Paris Agreement in 2015 and outlines the national emissions trajectory up to 2050. South Africa’s national emissions are expected to peak between 2020 and 2025, plateau for approximately a decade and decline thereafter in absolute terms. The Musina-Makhado project alone will contribute 6% - 10% of the emissions proposed in South Africa’s PPD that was used to inform the NDC, thereby significantly altering the national greenhouse gas trajectory that has been published and committed to. The IRP Draft Update 2018 36 makes allowance for two additional coal power stations to be commissioned. These stations are already in the planning stages. The power plant planned as part of the Musina-Makhado SEZ development would therefore require a Ministerial Determination before construction can begin. The update to the IRP aims to reduce the emissions of South Africa’s electricity generation sector by reducing the use of emission intensive technologies such as coal power stations. The addition of the power plant at Musina-Makhado would counter the objective of South Africa to reduce its emissions as a result of coal fired power generation. The effect of adding the Musina-Makhado SEZ power plant can be seen in the graph below which plots the emission intensity of the national grid as per the IRP Draft Update 2018.
36
It must be noted that at time of submission of this report to the Environmental Impact Practitioner, the IRP 2010-2030 was the binding IRP. Whilst due consideration was given to the provisions of the IRP 2010-2030, the provisions of the Draft IRP of 2018 was also considered in order to reflect government’s latest electricity considerations. At time of submission of this climate change impact assessment to the Environmental Impact Practitioner, it must be noted that the final version of the IRP 2019 had not yet been published, and as such the binding IRP applicable at time of conducting this climate change impact assessment, was the IRP 2010-2030.
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IRP 2018 CO2 Intensity 1.0000 0.9000 0.8000
kg CO2/kWh
0.7000 0.6000
Grid Intensity 0.5000 Musina-Makhado plant added intensity
0.4000 0.3000 0.2000 0.1000
2020 2021 2022 2023 2024 2025 2026 2027 2028 2029 2030 2031 2032 2033 2034 2035 2036 2037 2038 2039 2040 2041 2042 2043 2044 2045 2046 2047 2048 2049 2050
0.0000
Figure 14: Effect of the project on the IRP Global Context Climate change is a global phenomenon making it difficult to distinguish between local and international climate change drivers. Global anthropogenic climate change is caused by the accumulation of greenhouse gas emissions. The impacts of the Musina Makhado project will impact the global inventory particularly as the planned activities in the project are in emission intensive industries. This analysis is based on the assumption that the construction of the plants considered in this project will not increase the global demand for the metals to be produced. The increased demand will be driven by the growth of the new green economy, as shown in Figure 15 below. It is therefore assumed that production from the planned project would crowd out production from old plant with lower efficiencies, higher cost, and higher emissions. The World Bank conducted a study which revealed that increased commodities, particularly metals, will be necessary to achieve the various development objectives required by the Paris Agreement targets37. The increased demand for steel in three different emission reduction scenarios can be seen in the following figure.
37
World Bank, 2017. The Growing Role of Minerals and Metals for a Low Carbon Future, s.l.: World Bank.
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Figure 15: The growing role of steel for a low carbon future (2DS - 2˚C scenario. 4DS 4˚C scenario, 6DS - 6˚C scenario). Steel and other metallurgical plants generally have long life-spans. In this context, one of the biggest challenges in the decarbonisation of the world economy lies in the handling of the older, high emission plants. The construction of modern, low emission, plants is imperative if the world is to meet its emission reduction targets. In this context the construction of the SEZ could contribute to the decarbonisation of the global economy by introducing low emission plants. The difference between the emission intensities associated with the current fleet of metallurgical plant in the world, and the recommended intensities as per this report, for the volumes of production planned for this project, is shown in the last column of Table 14 below. Table 14: Comparison of current and required emission intensities. Plant Coal Washery Coke Plant Heat Recovery power generation Coal-fired power plant Ferrochrome plant Ferromanganese plant Silicon-manganese plant Carbon Steel Plant Stainless Steel Plant Lime Plant Cement Plant Sewage Treatment Plant Water Treatment Plant
Emissions based on 2010 historic intensities 900 ktCO2e/y * * 13.5 MtCO2e/y 2.2 MtCO2e/y 3.5 MtCO2e/y 7.2 MtCO2e/y 3.3 MtCO2e/y 1.1 MtCO2e/y 2 MtCO2e/y 99 tCO2e/y 212 tCO2e/y
Emissions based on 2°C target intensities for 2030 630 ktCO2e/y * * 10.1 MtCO2e/y 1.7 MtCO2e/y 2.6 MtCO2e/y 4.5 MtCO2e/y 2.3 MtCO2e/y 869 ktCO2e/y 1.6 MtCO2e/y 69 tCO2e/y 149 tCO2e/y
Difference 270 ktCO2e/y
3.4 MtCO2e/y 561 ktCO2e/y 863 ktCO2e/y 2.7 MtCO2e/y 1 MtCO2e/y 223 ktCO2e/y 406 ktCO2e/y 30 tCO2e/y 64 tCO2e/y
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Total SEZ
33.7 MtCO2e/y
24.3 MtCO2e/y
9.4 MtCO2e/y
If the plants in the SEZ are built to the intensities required to align with the 2°C target trajectory, as indicated in Table 14, then the SEZ could emit around 10 million tons CO2e less per year than if the plants are built according to current industry standards. This would lead to 24 million tonnes CO2e being emitted on an annual basis.
5.3 Impacts on Climate Change The high-level impacts from the perspective of the national and international greenhouse gas inventories do not necessarily reflect the impacts of the Musina-Makhado project from the domestic or global environmental perspective. Each participant in the global economy has a responsibility to minimise their contributions to climate change. Therefore, there is a collective responsibility to address climate change despite the inability to attribute specific greenhouse gas emissions from the project to specific effects on climate change. The impacts of the Musina-Makhado project’s greenhouse gas emissions have been assessed in Table 15, as per the Environmental Impact Criteria detailed in Section 4.1.2 of this report. The assessment results indicate that the activities undertaken in the project will produce greenhouse gas emissions that will contribute to the national and global inventories and climate change. Table 15: Climate change impacts of the Musina-Makhado SEZ Development emissions during operations Nature: The greenhouse gas emissions produced as a result of the industrial operations will contribute to the global phenomenon of anthropogenic climate change. Numerous global changes are likely to manifest due to climate change, although none that can be attributed directly or indirectly to the specific greenhouse gas emissions of any individual source, such as the proposed Musina-Makhado SEZ Development. The total Scope 1 and 2 emissions from the operational phase of the SEZ are calculated to be 727 million tCO2e38, which is 10% of the South African carbon budget of 7,572 MtCO2e. The total emissions from the industrial complex’s operation are therefore above the 0.13% ‘high’ rating threshold in relation to the national carbon budget, as set out in Table 8. Below illustrates the indicators with and without mitigation. As noted in Section 4.1.2, South Africa’s legal framework has yet to appropriately describe the magnitude of greenhouse gas emissions within the context of these environmental impact assessment reporting requirements. Without Score With Mitigation Score Mitigation Reversibility None 5 None 5
38
Using 2°C target intensities for 2030.
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Extent Duration Magnitude Probability Significance Status of impact Irreplaceable loss of resources? Can impacts be mitigated?
National/Internati onal Permanent Very High Definite High Negative Yes To a limited extent
5 5 5 5 100
National/Interna tional Permanent Very High Definite High Negative Yes To a limited extent
5 5 5 5 100
Mitigation: It is proposed that the environmental authorisations for the individual plants in the SEZ specify that the maximum emission intensities for the plants to be built is as would be required by the science based target trajectories for 2030. This recommendation is based on the required decarbonisation rate for the global economy as well as the assumption that the new plants will not be retrofitted during the first 10 years of operation. Cumulative impacts: The emissions from the operational phase of the mine are cumulative. The increase of greenhouse gasses in the atmosphere lead to an increase in global temperatures and resultant climatic changes. Residual risks: Greenhouse gasses have the ability to remain in the atmosphere over significant periods of time. This contributes to the rapid increase in global temperatures. The effects of these emissions are not immediately felt but are residual in that the impacts of climate change, as a result of the SEZ emissions, will remain even after the various activities within the SEZ have been decommissioned. The results of the above assessment, based on the provision in NEMA, indicate that the emissions from the project’s operations will have a High impact rating (significance score of 100). However, considering the tailored methodology developed for climate change specifically, the magnitude of the project impact is Very High. When considering the impact score for the construction phase, the impact score will always be High. This is independent of the magnitude of the GHG emissions, as the impact is still irreversible (score = 5), global in its extent (score = 5), is effectively permanent (score = 5) and has a 95% chance of occurring (score = 5). However, these emissions pale in comparison to the operational emissions that will result from the proposed SEZ and various activities planned within. Even with a low magnitude (score = 1), the significance will have a score of 80. There are options to mitigate the greenhouse gas emissions of the SEZ during the operational phase of the various activities. These options will not alter the impact of greenhouse gas emissions on climate change in terms of the extent, duration or probability of the impacts. Mitigation can only alter the magnitude of the impact primarily by reducing the quantity of greenhouse gas emissions.
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5.4 Project Alternatives To date detailed designs with regards to the various activity processes envisioned for the SEZ have not been available. A Greenhouse Gas Emission Indicators Report was provided by the Client. However, no indication of methodology, variables and input data were provided to unpack the emission intensities for a full comparison. In addition, the lack of design data and process details prevent an analysis of possible alternatives. This assessment therefore urges that the EIAs for the various activities within the SEZ consider appropriate alternatives in terms of project design to identify opportunities for potential mitigation alternatives related to emission intensities. As discussed, this report has suggested emission intensities in terms of a 2030 timeframe and best practice. Table 16 below provides a comparison between the 2010 benchmark intensities, proposed 2030 intensities as well as the emission intensities provided by the Client. The following must be noted: • The intensities for the Ferrochrome and Ferromanganese plants were adjusted using an energy intensity of 3.5MWh/tonne product39 and the South African grid emission factor of 0.911tCO2e/MWh. This allows the intensities to be accurately compared. The intensities for the silicon-manganese plant cannot be compared as the boundaries are unknown. The difference between the proposed 2°C target intensity for 2030 and the provided information warrants a review of the figure contained in the Greenhouse Gas Emission Indicators Report as provided by the Client. • The intensity for the cement plant was calculated based on the provided information. In comparison with the benchmark intensity, the intensity from the Greenhouse Gas Emission Indicator Report is much lower. It is therefore recommended that final EIA of the plant relook at this intensity. Table 16: Emission intensity comparison Plant
Coal Washery Coke plant Heat Recovery power generation* Coal - fired power plant* Ferrochrome plant Ferromanganese plant Silicon- manganese plant Carbon steel plant Stainless steel plant Lime plant
39
2010 Intensity
2°C target intensity for 2030
0.30
0.21
-
-
4.49 4.49 6.90 0.60 1.11 1.09
3.37 3.37 5.18 0.37 0.78 0.87
Intensity provided in Greenhouse Gas Emission Indicator Report -
4.51 4.19 1.32 -
1.00
Based on consultation with an international ferro alloys expert
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Cement plant Sewage Treatment plant Water treatment plant
1.00 0.0007 0.0007
0.80 0.0005 0.0005
0.26 -
Note: It was assumed that all electricity consumed by the plants in the industrial complex was produced by the onsite power plant. The Scope 2 emissions included in the calculations therefore relate to the electricity produced at this power plant. The emissions from the power plant are thus excluded to avoid double counting. The above table indicates that the emissions intensities, as provided, related to the Ferrochrome, Ferromanganese and Lime plants are above the suggested 2030 emission intensities. Therefore, these plants should consider mitigation actions as part of their current design processes to reduce their respective emission intensities in line with both local and global climate commitments. In terms of mitigating the impact of the emission intensities, as listed in Table 12 above, the following should be considered in the detail design of the various plants:
40 41
•
The production of ferrochrome, ferromanganese and steel results in off gas due to the processes used40. This off gas can be used in gas engines for power generation. This would result in less electricity sourced from a carbon emission intensive source such as a coal fired power plant.
•
Slag is a waste/by-product of the metal smelting process. This slag is often granulated using a water jet; a process which uses large volumes of water. This process also does not allow for the recovery of the heat generated. The cooling of one tonne of slag can release approximately 1.8GJ of heat. An alternative process can be used which is termed dry slag granulation41.
•
In dry slag granulation, the molten slag is subjected to centrifugal forces using a spinning disc which causes the slag to atomise. The slag is then quenched and solidified using air to recover the waste heat. This produces a product that can be used for cement manufacturing in addition to the recovered heat. The recovered heat can be used for several purposes including preheating and steam generation. This avoids emissions in two areas: those associated with clinker production for cement manufacture and the emissions from power generation if the heat is used to produce steam for a steam turbine.
•
Coke oven gas is produced during the manufacturing of coke. This gas has various uses which can contribute to reducing emissions and increasing efficiency. These include preheating the coke oven with the gas and using the coke oven gas for power generation. The gas can also be used in a blast furnace as a supplementary fuel.
•
Biomass can be used for power generation and is a less carbon intensive source than coal. This could be considered as an alternative for power generation in the Musina-Makhado SEZ making use of alien invasive vegetation in the area. Further investigation would be G. Ramakrishna et al, “Exergy and its Efficiency Calculations in Ferrochrome Production”, 2014, The Minerals, Metals &Materials Society and ASM International CSIRO, “Dry slag granulation: producing valuable by-products from waste”, 2 January 2019, Australia
65
required into the feasibility of this as it takes approximately 1 tonne of biomass per hour to generate 1MWh of electricity. •
Waste heat recovery can be implemented in the lime plant which can then be used for several other uses. These include using the heat for drying limestone and preheating in other plants. The heat can also be used for electricity generation which can then be used where required in the industrial complex to offset the electricity required of the emission intensive coal power plant.
Impacts of Climate Change on the Project Due to the interdisciplinary and cross cutting nature of climate change, climate vulnerability is not only caused by the level of exposure, but also by the social, economic, environmental and institutional contexts that interact with the changing climate. As a result, climate change impacts and risks cut across a number of sectors including the economy, the water sector and social ecosystems, illustrated below.
Negative impacts on each of the sectors has implication for the economy
Loss of ecosystems that provide valuable services
Food security can be aggravated by reduction in agricultural products, droughts and poor health
Climate Risks are cross-cutting through various sectors
People in settlements are exposed to heatrelated health impacts
Impact of extreme weather events on infrastructure, agriculture, settlements and health
Invasive plants and land-use change impact agriculture ecosystems
Water quality is directly linked to water-borne disease and impacts freshwater ecosystems
Water stress and increased sectorial competition for water
Figure 16: Climate risks impacting various sectors (adopted)42 42
Engelbrecht, F. & Davis, C. a. T. T., 2016. Climate Change over South Africa: From trends and projected changes to vulnerability assessments and the status quo of national adaptation responses, Pretoria: CSIR.
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South Africa is already experiencing detrimental climate change impacts. These include, for example, prolonged regional droughts and flash floods. Such events result in water constraints and operational stoppages in production and industrial processes. However, the most significant effects of climate change are likely to emerge over the medium to long term. The timing and magnitude of these effects are uncertain. To account adequately for the potential climate change effects in planning processes, companies need to consider how climate related risks and opportunities, as well as the associated impacts, may evolve under different conditions. The Vhembe District Municipality has acknowledged that climate change poses a threat to the development of the region, the environment and its residents. The proposed SEZ faces a number of these climate change related risks across its core operations, value chain, and broader network. The risks are classified as either low or high depending on the emissions scenario. Core operations for this assessment include the plants within the boundary of the proposed SEZ, as indicated in Table 2 in section 2.2. The core operations are expected to be exposed to both physical and transitional risks as a consequence of climate change. The value chain of the proposed SEZ is diverse and include a number of inputs such as water, diesel, coal, iron ore, and lime. For the purposes of this assessment, water will be assessed in more detail within the value chain under section 6.2 as it influences the majority the SEZ as a whole. Water is a key input for many of the industries within the SEZ and is significantly impacted by climate change. It is expected that the value chain will also be exposed to both physical and transitional risks as a consequence of climate change. Below outlines a climate change resilience assessment identifying the impacts climate change may have on the project.
6.1 Emission scenarios and impact analysis Emissions scenarios for this report are described by using Representative Concentration Pathways (RCPs) which are scenarios that include time series of emissions and concentrations of greenhouse gases, aerosols and chemically active gases together with land use/land cover. Each RCP scenario represents only one of many possible scenarios that would lead to specific radiative forcing, and therefore global warming, characteristics. Each RCP also emphasizes the trajectory taken over time to reach the outcome43. Four RCP’s are used in the Fifth IPCC Assessment26 as a basis for climate predictions and projections. The scenarios include a stringent mitigation scenario (RCP2.6), two intermediate scenarios (RCP4.5 and RCP6.0) and one scenario with very high GHG emissions (RCP8.5). Scenarios without additional efforts to constrain emissions (’baseline scenarios’) lead to pathways ranging between RCP6.0 and RCP8.5. RCP2.6 is representative of a scenario that aims to keep global warming likely below 2°C above pre-industrial temperatures. The RCP scenarios are consistent with the wide range of scenarios in the literature as assessed by IPCC working Group III on mitigation of climate change.
43
Moss et al., 2010, The next generation of scenarios for climate change research and assessment, Nature 463, 747 – 756.
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The two emissions scenarios considered in this assessment are: • No GHG mitigation scenario RCP 8.5: business as usual or baseline scenario where global average temperatures are expected to increase by 6 C from pre-industrial levels, which could, for example, increase the risk of heat stress. • Mitigation scenario RCP 4.5: intermediate measures are put in place with a view to limiting global average temperatures to 2 C. Focus was placed on these two scenarios due to the fact that the business as usual scenario give a good indication of how climate change would precipitate as a function of the current conditions. RCP 4.5 was selected as an intermediate scenario with a conservative representation of limited efforts to reduce global average temperatures. This is more consistent with most national policies which aim to effect limited change within one area of national life over a timeframe such as South Africa. It is important to note that different components related the SEZ (core operations, value chain and broader network) will experience risk differently and with varying impact. For the purposes of this assessment, risks have been classified as either physical or transitional (regulatory), as indicated in the recommendations of the Task-force on Climate-related Financial Disclosures. The relationship between physical and transitional risks under the unmitigated and mitigated emissions scenarios are typically inverse of one another, as illustrated in the following figure.
Figure 17: Forward looking scenario analyses44 Typically, physical risks are higher under an emissions scenario with low mitigation where few to no policies and measures are put in place to reduce emissions, resulting in increased physical impacts. Correspondingly, transitional risks would typically be low under an unmitigated emissions scenario, as transitional risks are generally associated with policy implementation aimed at adaptation. Conversely, physical risks are typically lower and transitional risks are higher under a mitigated emissions scenario. 44
Promethium Carbon
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The impacts of climate change are discussed further in relation to SEZ core operations, value chain and broader network below by considering temperature, water, social, biodiversity and transitional risk aspects.
6.2 Increased Temperature Climate change models predict that temperatures are to increase in the Limpopo province by as much as 2°C by 2035, by 1-2°C between 2040 and 2060 (or between 2-5°C in the high-end scenarios, RCP 8.5), and by 3-6°C between 2080 and 2100 (or 4-7°C in the high-end scenarios, RCP 8.5 )12. Rising temperatures would also result in an increase in the intensity and frequency of heat waves and wind speed. The culmination of these stresses can result in a greater number of people at risk of heat-related medical conditions as is discussed below. The Vhembe District Municipality has identified increases in temperature and the frequency of extreme weather evens as a developmental challenge within the Integrated Development Plan12. They have further indicated that climate change may make conditions more favourable for the incubation and transmission of waterborne diseases and disease carrying vectors. This could impact business continuity of the SEZ as a result of labourers falling ill and being unable to work.
.
Musina
SEZ Site
. .
.
Makhado
Senwabaranwa Mogwadi
.
. . .
Thohoyandou Malamulele
Giyani
Modjadjiskloof
Figure 18: Projected average temperate change for the period 2021 -2050, relative to the baseline period (1961 – 1990)27.
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From an operational perspective, heat stress directly impacts on labour productivity and is a major occupational health risk. High heat exposure restricts worker’s physical functions, their capabilities and ultimately work productivity and capacity. Globally, a temperature increase of 1.5˚C by the year 2100 could lead to a 2.2% drop in working hours which could result in a cost to the global economy of $2.4 trillion45. Increasing numbers of hot days, especially for people undertaking manual labour outdoors, will pose profound threats to the core operations of the SEZ in terms of occupational health and labour productivity. The can result in a loss of labour capacity which has further indirect impacts on the livelihoods of these individuals, their families and the communities as a whole, particularly those of which rely on subsistence farming46.
.
Musina
SEZ Site
. .
.
Makhado
Senwabaranwa Mogwadi
.
. . .
Thohoyando Malamulele
Giyani
Modjadjiskloof
Figure 19: Projected change in the number of very hot days (>35˚C) for the period 2021 2050, relative to the baseline period (1961 – 1990)27.
45
46
International Labour Organization, 2019. Increase in heat stress predicted to bring productivity loss equivalent to 80 million jobs, , viewed 26 July 2019, https://www.ilo.org/global/about-the-ilo/newsroom/news/WCMS_711917/lang-en/index.htm Watts, N., Amann, M., Ayeb-Karlsoon, S. & Belesova, K. e. a., 2018. The Lancet Countdown on health and climate change: from 25 years of inaction to a global transformation for public health. The Lancet, 10 February, 391(10120), pp. p.581-630.
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With regards to Vhembe District area, labour productivity is projected to decline significantly under a high emissions scenario. The figure below indicates the projected number of very hot days to increase to between 17 and 57 days under the worst case scenario RCP 8.5. Prolonged hot periods and increased temperatures may also reduce the operating efficiency of machinery or heavy goods vehicles. Equipment operating thresholds may be exceeded during episodes of extremely high temperatures. High temperatures could lead to extended use of air conditioners and ventilation systems within trucks and facilities operations. This will increase diesel consumption in the vehicles and electricity consumption in buildings.
6.3 Water related impacts Water security and groundwater are considered as part of this specialist climate change impact assessment. This is due to the fact that water is a key resource that will be affected as a result of climate change. In the case of the proposed SEZ, water is considered from a regional and international perspective as water is envisaged to be sourced from Zimbabwe. Water internationally The projected water use for the SEZ is estimated at 80 million m3/annum. This demand will create immense pressure on the local and cross-border water resources as well as the regional transferring catchments relevant to this study area. As indicated in section 2.3.3 a large portion of water is planned to be supplied by Zimbabwe. Table 17 below indicates the potential water resources within Zimbabwe considered to supply the SEZ. Time period Short term
Source Catchment Mzingwane
Medium term
Runde
Long term
Mzingwane Save
Details Beitbridge - Musina Integrated Water Supply Scheme - Potable water from Beitbridge water treatment plant - Raw water from Zhove via gravity for pick up at Beitbridge Tugwi- Mukosi Dam – A newly completed dam located 250 km from Beitbridge was identified as a potential project with surplus water that could be diverted to South Africa Thuli – Moswa Dam About 420 million m3 capacity dam upstream of Zhove Kondo – Chitowe Dam – The project will yield more than 820,000 ML. This dam site has a potential to sustain both Zimbabwean and South African water demand
Table 17: Potential source of water in Zimbabwe10
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Surface water in Zimbabwe accounts for 90% of the country’s supply47. Conversely there is very limited knowledge on how much ground water there is and the potential to utilise this water for the country’s needs. Nevertheless, the impacts of climate change in these catchment areas will impact both surface and ground water which will affect Zimbabwe as well as the SEZ which envisages to use water from Zimbabwe for day to day operations. In order to understand the impact on Zimbabwe’s water resources, the CSIRO Mk3 global circulation model (GCM) was used. The model indicates that under worst case and best case emissions scenarios, average annual precipitation will decrease in all of the Zimbabwean catchments except for Mazowe and Manyame which are predicted to remain relativity the same48. Runde and Mzingwane water catchment areas, which are sources of short and medium term water for the SEZ, will be affected the most. It is predicted the mean annual precipitation will decline in the region of between 12% for higher mitigation emission scenarios and 16% for lower emission mitigation scenarios by 2050. This significant uncertainty related to water supply poses a major risk to the SEZ. Climate change will also negatively impact the groundwater recharge rate for the areas and water supply for various water catchments. For limited or business as usual emission mitigation scenarios, precipitation would continue to decline for almost all catchment areas. On the other hand, for high emissions mitigation scenarios, affected water catchments such as Gwayi, Mzingwane, Runde, Sanyati and Save, could stabilise in terms of precipitation or start to recover between 2050 and 2080. An additional concern to the water resources of Zimbabwe is climate induced temperature increase. With Zimbabwe being heavily reliant on surface water for the country’s water needs, increasing temperatures will accelerate the rate of evaporation and impact surface water qualities in dams and rivers. In 2007, many dams were decommissioned due to evaporation of water resulting in dams running dry. With increasing temperatures predicted through to 2100 (Figure 7) evaporation has been estimated to intensify by between 4-25% on the river basins of Zimbabwe. This coupled with rainfall variability heightens water security risks and water supply risks to the SEZ. The implication of climate change on these catchments need to be considered in detail in terms of potential operational impacts on the SEZ and the water demand for both the Musina a Makhado Municipalities. Furthermore, water demand of the SEZ and the impact of climate change on above mentioned Zimbabwean catchments need to considered on the people living in Zimbabwe who are dependent on this water for their livelihoods.
47 48
D, Brown et al, 2012. Climate change impacts, vulnerability and adaptation in Zimbabwe, IIED Climate Change Working Paper. 4, December 2012.Viewed 26 July 2019 https://pubs.iied.org/pdfs/10034IIED.pdf R, Davis and R, Hirji 2014. Climate change and water resource planning, development and management in Zimbabwe, An issues paper, World Bank. Viewed 26 July 2019 http://documents.worldbank.org/curated/en/925611468329355687/pdf/937310WP0Box380babwe000Issues0 Paper.pdf
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This is particularly relevant as Zimbabwe is extremely vulnerable to the impacts of the climate change due to the fact that 62% of the total population reside in rural areas and are heavily dependent on climate sensitive water resources49. A report by the Southern African Development Community further supports this notion in which it found that the population of Zimbabwe is at very high risk of groundwater drought which could rise from 32% to 80% by 2100. Placing additional strain on the limited water sources, within the context of existing socio-economic vulnerabilities should be carefully considered and evaluated. Water locally The proposed SEZ falls within the Sand and Nzhelele catchment areas within the Limpopo Province. The Sand River catchment is the driest catchment area within Vhembe District Municipality. Surface water resources in the catchment area are limited to the small Seshego and Houtrivier dams and run-of-river abstractions. Groundwater is the only dependable water source for many rural settlements and villages with urban requirements being augmented from transfers from neighbouring Water Management Areas (WMAs). Table 18 indicates the Limpopo development level catchment water balances with no interventions. The Sand catchment indicates a negative water balance of -4.7 million m3/annum while the Nzhelele indicates a positive balance of 8.7 million m3/annum. The current surface water demand per capita for Makhado is 87.49 litres per person per day (l/p/d) with a supply of 91.83 l/p/d. Musina indicates a higher demand of 148.71 l/p/d and a supply of 283.21 l/p/d, illustrating that Musina is more dependent on surface water than Makhado 50 . An addition 80 million m3/annum will place major stress on the area’s available water resources. This additional water burden should also consider the potential urban expansion that would follow the development of the SEZ, placing further strain on the area’s water capacity. Table 18: Limpopo development level catchment water balances, 201051 Catchment
Water requirement Water availability (million m3/yr)* (million m3/yr) Matlabas 7 7 Mokolo 61.6 61.2 Lephalale 75.1 77.3 Mogalakwena 156.8 152.3 Sand 292.6 287.8 Nzhelele 39.4 48.1 Total 632.5 633.7 * Excludes IAPs and commercial forestry (streamflow reducers)
49 50
51
Water balance (million m3/yr) 0 -0.4 2.3 -4.5 -4.7 8.7 1.4
Chagutah, T., 2010. Climate Change Vulnerability and Preparedness in Southern Africa: Zimbabwe Country Report. Heinrich Boell Stiftung, Cape Town. Le Roux, A., van Niekerk, W., Arnold, K., Pieterse, A., Ludick, C., Forsyth, G., Le Maitre, D., Lötter, D., du Plessis, P. & Mans, G. 2019. Green Book Risk Profile Tool. Pretoria: CSIR. Available at: https://riskprofiles.greenbook.co.za/ Draft Reconciliation Strategy Report, 2016. Department of Water and Sanitation, Republic of South Africa P WMA 01/00/00/02914/11A. Viewed 10 June 2019 http://www6.dwa.gov.za/Limpopo/Documents/2016/Preliminary%20Reconciliation%20Strategy%20Report% 20Draft%2020160920.pdf
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The Vhembe District Municipality is currently experiencing issues of water scarcity and quality as all catchments in Limpopo excluding the Matlabas catchment indicate water quality issues that are expected to deteriorate over time. Climate change is expected to further exacerbate these problems as a result of increasing drought events. Under no mitigation scenario RCP 8.5, drought is projected to increase in the Musina and Makhado areas for the period 2035 – 2064. Increased drought would impact availability of water for the SEZ operations which is particularly of concern for the thermal plant and ferrochromium plant which require large amounts of water to operate. It is anticipated that SEZ will acquire energy from the thermal power plant, therefore, should the plant not be able to operate due to water constraints this will impact the entire SEZ’s productivity.
.
Musina
SEZ Site
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.
.
Makhado
Thohoyandou
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Senwabaranwa Mogwadi
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Giyani
Modjadjiskloof
Figure 20: Projected change in drought tendencies for the period 2035 - 2064, relative to the baseline period (1986 – 2005) under the low mitigation scenario RCP 8,527. A negative value is indicative of an increase in drought tendencies per 10 years Almost all of the provincial water resources have been fully developed and are allocated. Forty three per cent of the dams in the province have safety issues with additional issues of high water contamination impacting the quality of the water. With the SEZ predicted to be a large consumer of water, water availability and quality for other downstream uses become concerning, particularly in drought situations. The majority of the provincial water use demand is used for irrigation, mining and energy and some water to service rural areas12:
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Limpopo depends mostly on surface water sources, however, a large number of rural households depend on groundwater for domestic use. In 2011, 52,3% of Limpopo's population had access to piped water within their property, with almost a quarter of a million people not having access to formal water infrastructure. The following climate related risks have been projected for the Limpopo river basin12: • Decreased availability of water in rivers • Changes in the timing of high and low flows • A higher incidence of floods • Increased risk of water pollution and decreased water quality
.
Musina
SEZ Site
. .
.
Makhado
Senwabaranwa Mogwadi
.
. . .
Thohoyandou Malamulele
Giyani
Modjadjiskloof
Figure 21: Projected change in average rainfall for the period 2021 -2050, relative to the baseline period (1961 – 1990)27. A key challenge related to climate change, and specifically its impact on precipitation patterns, is the variability it could cause. In Limpopo there are indications that, in addition to prolonged periods of drought, the Province could also experience greater variability in rainfall (Figure 21) and extreme rainfall days (Figure 22). These intense rainfall days could result in flash flooding, which could cause both infrastructural, operational and labour safety damages.
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.
Musina
SEZ Site
. .
.
Makhado
.
Thohoyandou
.
Senwabaranwa Mogwadi
.
Giyani
Modjadjiskloof
Figure 22: Projected change in extreme rainfall days under RCP 8.5 for the year 205027. A value of more than 1 indicates an increase in extreme daily rainfalls In addition to the above, the water stress specifically related to climate change, for the proposed SEZ, was assessed using the World Resources Institute’s (WRI) Aqueduct tool 52 . Projected changes in water availability or impacts on water resources show how development and/or climate change are expected to affect water stress in a particular area. Water stress is the ratio of total withdrawals to total renewable supply in a given area. The WRI Aqueduct tool uses twelve different risk categories including physical, regulatory and reputational risks to determine water risk. Reference is also made to the baseline status and overall water risk of a particular area. The WRI Aqueduct indicates that the overall water risk of the area in which the proposed SEZ is situated, is “Medium Risk”.
52
World Resources Institute, n.d. World Resources Institute Aqueduct: Measuring and Mapping Water Risk, viewed 6 June 2019: http://www.wri.org/our-work/project/aqueduct
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SEZ Site
Figure 23: SEZ - overall water stress52. The overall “Medium Risk” rating indicates, as per earlier comments in this section, the possibility of process disruptions and the reduced availability of water which could interrupt the operation of the metallurgical plants in the SEZ. Therefore, water scarcity issues pose a critical concern from an operational point of view. In addition to the overall water risk, water storage was assessed for the purposes of this study. Water storage relates to the water storage capacity upstream of the proposed SEZ relative to the water supply to the facility. In terms of the proposed SEZ, water storage is classified as “Medium to Low”, which means that the availability of buffer capacity to withstand variation in water supply is at risk in the area. Furthermore, surrounding areas to the west of the proposed SEZ indicate as having “Low” to “extremely low” capacity for buffering in case of variations of water supply including for droughts or floods.
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SEZ Site
Figure 24: SEZ - upstream storage52. Under existing water constrained considerations and due to a low buffering capacity of the area, water stress could lead to social and environmental pressures on the proposed SEZ. Furthermore, increased competition for water within the District and across municipal areas could increase water pressure on the proposed facilities and can therefore have impacts on the operation. The SEZ will increase pressure on water availability for the surrounding municipalities due to the large demand from the SEZ. It is therefore crucial that the water balances for the SEZ and the surrounding area are determined for current and future use and importantly, the impacts of climate change on this demand be considered. An additional key climate risk associated with water in the area pertains to inter-annual variability. Figure 25 below indicates that the SEZ falls within an area with a high risk in terms of water supply year on year. This carries with it significant consequences for the area as well as the SEZ as water supply will fluctuate. Furthermore, climate change is expected to exasperate these issues through various extreme weather evens such as drought and high frequency rainfall periods.
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SEZ Site
Figure 25: SEZ - inter annual variability52. This again highlights the importance of a thorough water balance for the area which is cognisant of all these climate change water risks, now and in the future. Further consideration should be given to worst case scenarios and water alternatives in the episode of extreme weather events. This is to ensure that one caters for water risks at a regional scale and that the impacts of climate change are buffered and limited. It is therefore critical that the Environmental Impact Assessment, to be undertaken for each of the individual plants to form part of the SEZ, must prepare a water balance which takes cognisance of climate change and climatic modelling for the area. Physical risks within the value chain As indicated above, the intensity and variability of rainfall is increasing, meaning that even though rainfall events will be unpredictable, when they do occur, they will be more intense than normal. Such events could damage or wash away infrastructure or transport routes. This could negatively impact logistics, labour and the supply of products such as diesel, coal, iron ore and lime to the SEZ. The risk of supply chain disruptions for the construction phase of this project is medium, as the project is situated within a mining area which has sufficient stock levels of construction materials. The increased probability of storms may however impact the SEZ in terms of employee safety, infrastructure safety, production delays and increased insurance costs. Based on information available for this study, it is assumed that the electricity for the construction phase will be supplied by Eskom. During the operational phase electricity will be provided by the thermal power plant. In terms of climate change impacts, there are two key considerations with regards to electricity derived from Eskom: the first being water and the second being the regulatory implications of the proposed carbon tax on the power utility. 79
During 2017 Eskom consumed 1.43 litres of water for every kWh of electricity produced53. The bulk of the Eskom power stations are situated in the Mpumalanga region which is a water stressed province. The overall water stress, as determined by the WRI Aqueduct, of the Mpumalanga region is “Medium to High” and is shown in the following Figure 26 below. In addition, climatic models predict that the province is going to become increasingly drier and hotter.
Figure 26: Overall water stress in Mpumalanga region52. Water scarcity and increasing constraints in terms of access to water could negatively impact Eskom’s functionality. In turn, disruptions in Eskom’s ability to generate power could negatively impact on the construction of the proposed SEZ’s. Disaster risks – flash flooding The Makhado Local Municipality has seen an increase in the number of climate related disaster incidents over the past two years. This comes as a testament to the nature and variability that climate change imposes.
53
Eskom, 2018. Eskom Integrated Annual Report, Johannesburg: Eskom.
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800 714 700
Incidences
600 500 400 300 188
200 100 0
50 21 Fire
Storms/Floods 2016/17
2017/18
Figure 27: Disaster incidences from 2016 - 201854. Climatic models for the Limpopo Province together with the WRI Aqueduct Tool indicate water as being a high-risk resource, especially in the context of climate change. Climate change impacts in the Limpopo Province include an increase in the number of extreme rainfall events- hailstorms, damaging winds, thunderstorms and flooding. This is due to the fact that even though the region is becoming dryer, the intensity of extreme rainfall days increases. From Figure 10 in section 3.3.2.2 it is evident that the proposed SEZ is located in a medium to low flood hazard area. However, with a predicted increase in extreme rainfall days under RCP 8.5 for the period 2050, the risk of flash floods could pose significant risks to the safety of employees as well as causing operational disruptions at the SEZ which could lead to reduced output. Climate change will also increase the amount of energy storms have, enabling them to carry more water, have higher wind speeds and/or travel further. This increases the chance of severe storms, such as a tropical storm, coming far enough inland to cause severe rainfall and flooding in the area. Furthermore, water is required for the facilities to function and is a key consideration in terms of employee and community safety. As such, it will be critical for the proposed SEZ to develop sufficient water buffering measures and water recycling methods to ensure the operations are sustainable. It is clear from the above, that the region is facing considerable climate change related disasters and the operations of the SEZ would need to be conducted in such a manner as to buffer against the effects that climate change may pose by implementing risk mitigation and adaptation actions.
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Makhado Local Municipality, 2018. Makhado Local Municipality Draft Annual Report 2017/2018, s.l.: s.n.
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6.4 Social Impacts The social context as part of this study refers to communities / settlements (both urban and rural) that would be impacted, both directly and indirectly, by the SEZ from a climate change point of view. In this regard the Vhembe District Municipality is an appropriate administrative boundary to define the social environment for the purposes of the climate change impact assessment for the proposed SEZ.
South Africa is particularly vulnerable to climate change because of its dependence on climatesensitive economic sectors, high levels of poverty and the inter-related impacts of community health and service delivery challenges. Furthermore, climate change impacts and extreme weather events can affect some people or societal groups more than others. The extent to which a person or a group will be affected will depend not only on their exposure to the event, but also on their social vulnerability to change in climate – that is, how well they are able to cope with and respond to events like flash floods, drought and heatwaves as discussed in this report. Causes of social vulnerability to climate change in the case of the Musina and Makhado Local Municipality include, among others, informal housing, poverty, a high dependency ratio and limited/insufficient social infrastructure. The analysis undertaken for this climate change impact study shows two key trends of specific relevance to socio economic context of the Vhembe District Municipality: declining rainfall patterns for the area and an increase in daily minimum average temperatures. These two trends will have a particularly challenging impacts on the Local Municipalities and their communities due to the prevalence of vulnerable groups within the area. The health impacts of extreme heat range from direct heat stress and heat stroke, to exacerbations of pre-existing heart failure, and even an increased incidence of acute kidney injury from dehydration in vulnerable populations. Elderly people, children younger than 12 months and people of poor health are particularly sensitive to these changes55. In addition to the above, prolonged dry periods and a lessening of annual rainfall could constrain water service delivery and limit access to potable water, specifically within informal communities. Makhado has the second highest number of informal dwellings in the Vhembe district illustrated in (Figure 28).
55
Watts, N., Amann, M., Ayeb-Karlsoon, S. & Belesova, K. e. a., 2018. The Lancet Countdown on health and climate change: from 25 years of inaction to a global transformation for public health. The Lancet, 10 February, 391(10120), pp. p.581-630.
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Figure 28: Percentage of households in informal dwellings in the Vhembe District Municipality12. Limited access to potable water, exacerbated by informal living conditions in some areas, could lead to an increased spread of water-borne diseases through unhealthy living conditions severely impacting existing vulnerable groups. The relevance of these issues with regards to the proposed SEZ is that the Makhado Local Municipality has identified the industrial development as an economic opportunity for the area. As such, vulnerable communities will increasingly look to these industries for solutions, increasing social pressure and potentially impacting on the SEZ’s social license to operate. In addition, due to the location of the SEZ, it could attract large numbers of migrant workers, further exacerbating current service delivery constraints within the District and Local Municipalities. Description of local municipality socio-economic vulnerabilities The Vhembe District Municipality is made up of four Local Municipalities, Musina, Makhado, Thulamela and Mutale. The Vhembe District Municipality is located in Limpopo which is South Africa’s 5th largest province with a total land area of 125,755 square kilometres. The Vhembe District has a large agricultural economic sector and its rural population is dependent on agriculture for subsistence. Mining is the major economic driver in the province and contributes to more than a fifth of the province's economic growth. Approximately 1,294,722 people currently reside within the municipality and based on the vastness of the rural populace the municipality can be classified as predominately rural. Makhado has a greater population (558890) compared to Musina
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(114690) 56 . An overview of key demographic details within Vhembe District Municipality is presented in Table 19 below. Table 19: Vhembe District Municipality key demographic information (2011)12. General Information
Vhembe District Municipality 1,294,722
South Africa
34.88% 58.9% 17.11% 6.27%
29.17% 44.30% 21.19% 5.34%
69.9%
52.7%
Employed Not economically active Unemployed Discouraged work-seeker Education (aged 20 +) Post School Qualification
24.85% 50.79% 15.68% 8.68%
38.87% 39.21% 16.50% 5.41%
8.24%
9.94%
Grade 12/Matric High School Less than High School Other Vulnerability Indicators Household Dynamics Households
21.6% 33.39% 15.48% 21.63%
27.83% 32.16% 16.43% 13.64%
335,271
14,450,151
41.00%
20.56%
18.93%
16.32%
21.51%
12.20%
Population Age Structure Population under 15 Population 15 to 64 Population 40 to 64 Population over 65 Dependency Ratio People in age group 0-14 & 65+, supported by age group 15-64 Employment (between 15 and 64)
Percentage households involved in agricultural activities Dwelling Type Health Percentage of young (<5yrs) and elderly (>64yrs) Percentage workforce employed in the informal Sector
51,770,553
Key trends related to socio-economic context of the local municipality include the following: • As evident in Vhembe District Municipality’s Climate Change Vulnerability Assessment and Response Plan, climate change will impact the municipality’s Local Economic 56
MMSEZ Progress Report Musina 16 July 2019. Musina-Makhado Energy and Metallurgy Special Economic Zone, Socioeconomic impact assessment. Demacon.
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Development Strategy. With the municipal population growing, further pressure will be placed on the demand for services and the overall regional economic base. This is especially the case in the agriculture, industrial and mining sectors which have been identified as key economic focus areas for the district. •
In terms of climate change, long-term hotter and drier conditions could negatively impact the agricultural sector and have further consequences on all communities which are dependent on agriculture for their livelihoods.
•
There is a high dependency ratio within the Vhembe District Municipality. A high dependency ratio indicates that the economically active portion of the population in the municipality face a greater burden to support and provide the social services needed by those who are not economically active. Climate change will further increase the pressure on the portion of the population which is economically active through extreme weather events and thereby further increase the vulnerability of these communities.
The above-mentioned trends and related challenges, in terms of the impacts of climate change, can be exacerbated by high levels of poverty within the area. The population living in poverty is illustrated in Figure 29.
SEZ Site
Figure 29: Population living in poverty57.
57
SA Risk and Vulnerability Atlas, 2019. Socio-economic landscape. Viewed 11 June 2019 http://sarva2.dirisa.org/atlas/socio-economic
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According to the Makhado Local Municipality’s Integrated Development Plan for 2018/19, 45.4% of the population were living in poverty in 2011 58 . This is an indication of a high level of community vulnerability within the area and the subsequent need for food and job security. Climate change will directly affect the sectors upon which the poor are dependent, which in this case is mining, agriculture and tourism and should be considered in this regard. SEZ community vulnerability drivers Vulnerability drivers impact the exposure, sensitivity and adaptive capacity of systems. The following are relevant vulnerability drivers for consideration pertaining to the proposed SEZ’s communities and social aspects discussed above: •
Health - The health and safety of SEZ employees and the wider communities can be affected both directly and indirectly by a changing climate. Informal or less formal areas in the Vhembe District are specifically vulnerable to the spread of disease which can be driven by climate change. Long-term heat exposure can also exacerbate chronic diseases, including cardiovascular and respiratory disease, through indirect microbial and vectorborne pathways. Considering the backlog in service delivery; limited formal infrastructure and a growing population, the impact that climate change can have with regards to disease incidence is of a particular concern. This may impact SEZ employees who come from these areas and thus can have an impact on the operations of the SEZ.
•
Wildlife and agriculture – Wildlife and agriculture is an important economic sector within the Musina and Makhado areas. The proposed SEZ site is surrounded by wildlife tourism and agricultural practices, ranging from commercial to subsistence-based practices. Changing climatic conditions will impact the ability of the already vulnerable surrounding communities to develop alternate or subsistence-based means of income. Social unrest and community dependency on the proposed SEZ could impact the operations and increase unplanned social expenditure
•
Water - Water is an essential community service and essential for community wellbeing. With projections of increased rainfall variability, increasing drought occurrences, increase in clean water scarcity and an overall prediction of decreasing rainfall as described in section 6.2, climate change threatens the wellbeing of surrounding communities.
•
Living conditions - The less developed nature of settlements, such as some of the communities surrounding the proposed SEZ in the Makhado and Musina Local Municipalities, are characterised by service delivery pressure. This is further heightened by tensions around the need for a better quality of life and living condition. In this regard it is critical to consider the social context in terms of understanding potential operational risks that the SEZ are exposed to.
As such, based on the above vulnerability drivers, there are three key issues which could influence the proposed SEZ once operational. These are summarised as follows: 58
Makhado Local Municipality, 2018. Makhado Local Municipality Integrated Development Plan 2018-2019 Review, s.l.: s.n.
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•
Amplified community dependence on the SEZ for service delivery. This could increase social expenditure and result in unsustainable social spending and the possible stimulation of unsustainable growth of this area.
•
Strained service capacity, for example due to possible in-migration to the area and as a result of climatic events which has result in resource shortages. Water is a particularly sensitive resource within the area which is categorised as water stressed. Additionally, water impacts, either upstream or downstream from the SEZ’s operations, could result in community volatility and reputational damage to the SEZ. Furthermore, such volatility is not limited locally as water supply is planned to be source from Zimbabwe and thereby having international consequences.
•
Negative impacts on well-being of employees in terms of climate related impacts could result in a less productive workforce. As described earlier, vulnerable communities are more susceptible to climate induced livelihood impacts such as disease spread, heat stress and clean water scarcity due to drought and low rainfall.
Related to the above key issues, the following table (Table 20) provides an overview of the climate change manifestations, impacts on the broader network of the SEZ and the typical impacts that these could have. Table 20: Climate change manifestation, community impacts and operational influence59
Declining annual rainfall.
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➔
Increased energy demand for cooling.
➔
Declining air quality in the community – dust pollution if not adequately controlled and managed.
Dangerous working conditions
Reputational damage
Community volatility
Operational efficiency
Impact ➔ Increased temperatures become dangerous for workers
Increased social expenditure
Climate change manifestation High daily maximum averages coupled with increasing daily average minimum temperatures.
Increased community dependence
Possible SEZ Impacts
➔
Increased water demand.
➔
Water quality problems.
Promethium Carbon assessment
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Reduction in quality of life of adjacent communities.
➔
Adverse effects on water supply.
➔
Increased risk of death, injury, loss of property, and disease.
➔
Increase in the variability of daily rainfall – higher daily average rainfall and expected to be more intense.
➔
Displacement of people and migration to urban areas.
Community challenges could impact political and economic decisions and give rise to protest and unrest at the SEZ. This could affect operations and the work force, as well as the project’s social license to operate. As such, the impacts of climate change on the adjacent communities to the SEZ must be considered in terms of the physical risk considerations. Human Health Health is highlighted as a priority area of intervention in the Limpopo province due to the high levels of vulnerability to climate change. Of particular concern is the increase in temperatures which will have multiple health impacts and implications. For example, an increase in temperatures could lead to heat stress and dehydration. This will need to be considered by the SEZ as such conditions make the working conditions unsafe and unproductive. Increase in temperatures is also likely to cause an upsurge in vector borne diseases from the spread of mosquitoes, ticks, sand-flies, and blackflies. Rising temperatures will also cause an escalation of water borne and communicable diseases (typhoid fever, cholera and hepatitis). These diseases will affect the SEZ’s labour force and influence the productivity of the facility. Within the Vhembe District there are 21.51% percent of working individuals employed in the informal sector. As a result, the municipality has identified ‘Increased Occupational Health’ problems associated with temperature increases as a high sensitivity indicator due to the fact that the district has a low adaptive capacity to deal with these increases. Increased temperatures and extreme events such as heat waves are also likely to increase illnesses and injuries, especially for the Vhembe District which has a large proportion of the population having contracted HIV/AIDS and a high proportion of elderly in the area.
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SEZ Site
Figure 30: Vhembe district Municipality Percentage of Young (<5yrs) and elderly (>64yrs)12. Climate change impacts will also affect the provision of health services that communities in the district rely on. The district already experiences the following challenges with regards to provision of health services12: • • • • • • • •
Lack of basic amenities including shade at clinic visiting points; shortages of medicine; Lack of dedicated pharmacists and assistant pharmacists; Influx of migrants from neighbouring countries; Malaria; Rabies; HIV and AIDS; Tuberculosis; and Poor road and communication networks to access healthcare.
These challenges in the provision of health services may become exacerbated by climate change impacts, where for instance extreme weather prevents can delay or prevent the distribution of necessary medication. Human settlements Climate change will have various impacts on human settlements. Increases in the severity of storm events and flooding could damage strategic infrastructure which may result in a loss of industrial productivity and service delivery disruptions. In terms of access to services in the district, the
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majority of households live in formal dwellings, with 2.43% of households living in informal dwellings and 9.48% living in traditional dwellings. The impacts of storm events will particularly affect communities located in informal settlements around the SEZ. Households within flood plains where there is poor drainage infrastructure are particularly at risk, as communities will face damage as a result of flooding. Rural communities may also become more physically isolated due to extreme events impacting on key infrastructure, leading to increase trends of migration to urban and peri-urban areas. This may have an impact on the SEZ’s labour force, as workers might not be able, or be willing to travel from developed urban areas to the SEZ. Water and sanitation Vhembe District Municipality is currently experiencing issues of water scarcity and quality. Climate change is expected to exacerbate these problems. Drought, reduced runoff, increased evaporation, and an increase in flood events will impact on both water quality and quantity. Enhanced evaporation rates have caused deterioration in water quality due to increased salt concentrations in dams, wetlands and soil/plant systems. Increased drought means less water is available to dilute wastewater discharges and irrigation return-flows to rivers. This results in reduced water quality and associated downstream health risks to aquatic ecosystems. These concerns result in less water being available for irrigation and drinking purposes, which impact negatively on the livelihoods of communities, especially in rural areas. The Vhembe District Municipality is both the Water Services Authority and Provider. The main water challenges for the district include: the high water and sanitation backlog, upgrading of infrastructure, resource extension, operation and maintenance, as well as refurbishment needs. 27.93% of the district municipality’s community lack access to piped water12. Furthermore, the Vhembe District Municipality’s wastewater management has been assessed to be in a “critical” state, as the district received a 16.30% Green Drop System audit in 2011 12. Additionally, there were no clean audits on municipalities in the Limpopo Province for the 2017/18 financial year which further highlights issues around water management in the area60. Critical state systems are more susceptible to the impacts of climate change where droughts will exasperate these issues through less water availability and as a result further impact the livelihoods of communities in the Vhembe District and therefore impact the SEZ. In-migration risks It is not only communities in close proximity to the SEZ that will be impacted as a result of climate change. The SEZ is strategically located in terms of access to South Africa’s neighbours. The scale of the development, considering the social vulnerability of countries such as Zimbabwe and 60
Daily Maverick, 2019. ‘It’s a systems breakdown across the country, with only 18 out of 257 municipalities receiving a clean audit., Viewed 26 July 2019 https://www.dailymaverick.co.za/article/2019-06-27-its-a-systems-breakdownacross-the-country-with-only-18-out-of-257-municipalities-receiving-a-clean-audit/
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Mozambique, could attract large number so migrant workers. Climate change is likely to particularly affect socially vulnerable populations already inclined to migrate. Climate-related food insecurity, service incapacity and climatic impacts on subsistence based livelihoods lead to increased migration. The following figure illustrates climate related events and their impacts on Southern African countries.
Figure 31: Summary of the climate-related events per country in southern Africa since 198061 Although South Africa has the highest number of recorded climatological events and the highest economic cost of damages, the communities of Mozambique, Madagascar, and Malawi are particularly vulnerable to extreme climate events62. Mozambique is one of Africa’s most vulnerable countries to climate change. Poverty, weak institutional development and frequent extreme weather events make Mozambique especially vulnerable62. Climate related hazards such as droughts, floods and cyclones are occurring with 61 62
CSIR, 2017. Climate Risk and Vulnerability: A Handbook for Southern Africa (2nd Edition). Davis-Reddy, C.L and Vincent, K Netherlands Commission for Environmental Assessment (Dutch Sustainability Unit). Climate Change Profile: Mozambique.
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increasing frequency. This has a negative impact on a population that is already vulnerable in terms of institutional and infrastructure readiness. Central Mozambique is projected to experience recurrent agricultural losses as a result of droughts, floods, and uncontrolled bush fires. The densely populated coastal lowlands will be increasingly affected by erosion, saltwater intrusion, loss of vital infrastructure and the spread of diseases such as malaria, cholera and influenza62. Zimbabwe will face increasing drought conditions62. This will have a severe impact on the country’s agricultural base and related capacities. Coupled with increasing socio-economic pressures and struggling institutional capacities, this country’s population will be prone to migration. The strain on communities in Mozambique and Zimbabwe as a result of climate change could increase migration to areas such as the local municipalities surrounding the SEZ. This could lead to community tensions as competition for land, water and basic services increase, further increasing the existing vulnerability of the local communities.
6.5 The Natural Environment Ecosystem services, similar to the issue of water within the context of climate change and the nature of climate change impacts, is addressed from a regional perspective. Ecosystem services play a vital role in climate change adaptation, as such, it forms part of this climate change impact assessment. Ecosystem services, are considered to be ‘nature’s contribution to people’, and can include the following functions63: • Habitat creation and maintenance of genetic diversity; •
Moderation of extreme events: wetlands regulate flood waters and trees stabilise slopes and prevent erosion while maintaining soil fertility;
•
Soil pollination reduction, plant propagation and biological control of pests and vector borne diseases;
•
Regulation of climate: trees provide shade and regulate air quality by removing pollutants from the atmosphere;
•
The provision of food, feed, energy, fresh water and raw materials;
•
Physical and experimental interactions with nature, symbolic meaning and inspiration.
Climate change as well as human activities are direct drivers of ecosystem change and could significantly impact vulnerable people, who often rely heavily on natural systems64. Therefore, a disruption in ecosystem services due to climate change can have an impact on the people who rely 63 64
Pascual, U. e. a., 2017. Valuing nature’s contributions to people: the IPBES approach. Current Opinion in Environmental Sustainability, Volume 26, pp. 7-16. Howe, C. e. a., 2013. Elucidating the pathways between climate change, ecosystem services and poverty alleviation. Environmental Sustainability, Volume 5, p. 102 – 107.
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on the ecosystem for their livelihoods. This is reiterated within the Vhembe District Municipality Climate Response Plan which indicates that the aquatic and terrestrial ecosystems of the Limpopo province are highly vulnerable to the impacts of climate change5 and as a result exposure them to impacts which affect their livelihoods. The degradation and loss of ecosystem services will most likely affect lower income and vulnerable people disproportionately and has the potential to be a significant barrier to reducing poverty 65. The loss of natural systems as a result of climate change impacts in the region will exacerbate social vulnerabilities and could further increase the pressure on the proposed SEZ’s social licence to operate.
Land is a finite physical asset and cannot be reproduced. The latest IPCC report on land and climate change notes that land is both a source and a sink of greenhouse gases (GHGs) and plays a key role in the exchange of energy, water and aerosols between the land surface and atmosphere66. Land ecosystems and biodiversity are vulnerable to ongoing climate change and weather and climate extremes, to different extents. The report found that changes in land cover and the loss of natural vegetation, could affect regional climate and result in, inter alia, accentuated warming and increased intensity, frequency and duration of extreme events66. As mentioned, land is both a CO2 sink as a well as source of CO2 emissions as a result of land use change activities, such as infrastructure development. In this regard the loss of natural land cover contributes to climate change in two ways: Firstly, the loss of natural vegetation results in the loss of a natural carbon sink. Secondly, the use of land for large-scale development, such as the Musina Makhado SEZ, results in increased emissions. In addition, the loss of large tracts of land in terms of vegetation cover, could exacerbate existing land impacts related to climatic changes. Increased land surface air temperature and decreased precipitation, in conjunction with climate variability and human activities such as increased land use change through development, have contributed to desertification, specifically in the Southern African context. In addition, climate change can worsen land degradation through increased rainfall intensity, drought and heat. These climatic parameters are expected to manifest in the Vhembe District Municipality as a result of climate change. Biomes and ecosystem services Vhembe District has a range of diverse ecosystems which support many threatened flora and fauna. These ecosystems include savanna, grasslands, indigenous forests, mountain escarpments (Soutpansberg) and numerous wetlands including a RAMSAR Wetland (Makuleke Wetland) in the North Eastern part of the Mutale Local Municipality. The savanna biome covers approximately 65
66
Millennium Ecosystem Assessment, 2005. Ecosystems and Human Well-being: Synthesis, Washington, DC: Island Press. IPCC, 2019. IPCC Special Report on Climate Change, Desertification, Land Degradation, Sustainable Land Management, Food Security, and Greenhouse gas fluxes in Terrestrial Ecosystem: Summary for Policy Makers. Intergovernmental Panel on Climate Change.
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98% of the Vhembe District Municipality with the remainder being made up of forest (1%) and grassland (0.2%) biome. The impacts of climate change on South African biomes is depicted in Figure 32 below. The climate projections range from current, low (wet/cool climatic conditions), intermediate (median temperature and rainfall predictions) to high (dry/hot climatic conditions) scenarios.
Figure 32: Bioclimatic envelope projections to 205022. Common under each projection is that the climate envelope in Limpopo is likely to resemble a different biome in future. This means that the endemic biota of the biome could experience significant climate-related stresses. As illustrated in Figure 32 above, the Grassland biome is likely to decline in the future across all the scenarios with the Savanna biome increasing in size. As a result, South Africa has identified Grasslands as the highest priority biome in terms of protection, restoration and conservation22. For the Limpopo and the Vhembe District however, Grasslands currently only contribute a small portion of the area and therefore these areas will not be as greatly impacted as opposed to for example, the Mpumalanga province. However, from a broader context, bush encroachment of woody plants into Grassland areas which are situated in water catchments 94
may have an impact on water supply as this water management area transfers water to Limpopo. This will therefore also have implicated which impact water supply to the Vhembe District.
Importantly, the unique biodiversity of the Vhembe District lends itself to the establishment and growth of South Africa’s biodiversity economy. Within South Africa, the biodiversity economy refers to the economic activities that either contribute to environmental conservation through their activities or activities that directly depend on the biodiversity for the core of their business67. In the development of a successful biodiversity economy within South Africa, three key economic subsectors have been focused on, namely: wildlife awareness and viewing, bioprospecting and, ecotourism. All three of these subsectors result in great benefits to local communities (by providing job opportunities), sustainable utilisation of the resources and surroundings, as well as overall economic development and transformation. The transition of such communities and affected areas into sustainable and economically stable hubs of interest leads to valuable economic growth of the country with relatively low initial expense and an easily facilitated community involvement requirement 68. Bioprospecting is the search for the discovery of new medicinal drugs and various other valuable compounds that may result from animal and plant species. Wildlife commercialisation includes the correct and sustainable development of game and nature reserves. The presence of such reserves would lead to protection and study of wildlife in their natural habitats, ensuring minimal disruption and unnecessary harm to the wildlife 69 . Eco-tourism is another type of tourism that enables economic growth while ensuring conservation of various biodiversity nodes and preserving the ecosystems, while still allowing economic growth of an area70. The wildlife and bioprospecting sub-sectors have added significant potential growth for the future economy in South Africa. The contribution of these sub-sectors is measured according to the Gross Domestic Product (GDP) growth and their relative contribution to the GDP. These economic activities linked to biodiversity are critical in building climate resilience in vulnerable communities. It also assists with the safeguarding of environmental and ecosystem related infrastructure critical to both mitigating and adaptation to climate change. In considering these elements within the context of the Vhembe District, based on existing climate change trends and projected climate change patterns, it is evident that biodiversity will be significantly impacted by climate change. Subsequently, the potential economic and social benefits associated with the maximising of ecosystems and biodiversity could be lost. This will significantly hamper the adaptive capacity of the area in terms of climate change. 67
Department of Environmental Affairs, 2016. National Biodiversity Economic Strategy [Online] Available at: https://www.environment.gov.za/sites/default/files/reports/nationalbiodiversityeconomystrategy.pdf [Accessed 5 March 2019]. 68 Explore South Africa, 2018. The biodiversity economy. [Online] Available at: http://www.exploreonline.co.za/articles/the-biodiversityeconomy-26212.html [Accessed 5 March 2019]. 69 Department of Environmental Affairs, 2016. National Biodiversity Economic Strategy [Online] Available at: https://www.environment.gov.za/sites/default/files/reports/nationalbiodiversityeconomystrategy.pdf [Accessed 5 March 2019]. 70 The International Ecotourism Society, n.d. About Us. [Online] Available at: https://ecotourism.org/what-is-ecotourism/ [Accessed 13 February 2019].
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Drought Increased frequency of veld fires associated with drought induced winds have shown to destroy entire habitats and threaten the biodiversity of these ecosystems. As a result, decreased rainfall events resulting in drought has been identified as an indirect threat to biodiversity in the Vhembe District12. This has been exasperated by the limited supply of ground and surface water in the District as well as increasing water demand for domestic, agricultural and mining purposes. Furthermore, it has been noted by the Vhembe District Municipality that existing water resources are being polluted by poor land management, poor sewage systems and agricultural pesticides resulting in less usable water. These issues will be of greater concern should the SEZ abstract ground and surface water from local water resources and thereby further limiting the amount of available water for the area.
6.6 Transitional Risks The proposed SEZ tenants will have regulatory obligations associated with greenhouse gas emissions. Non-compliance with these regulations will carry penalties that will range from fines to criminal prosecutions. Once operational, the SEZ tenants, as per the current Master Plan, will need to develop mandatory pollution prevention plans in accordance with the National Pollution Prevention Plans Regulations71, published under the National Environmental Management Act: Air Quality. The SEZ will also be liable for reporting as per the National Greenhouse Gas Emissions Reporting Regulations72. In this event, the SEZ tenants will also be liable for carbon tax73. The gross tax rate for 2019 was R 120/tCO2e, however there are provisions for various allowances which reduced the effective tax rate to R 36/tCO2e. The second phase of the Carbon Tax will include a linkage to the national sectoral emission targets being developed by government. Once finalised, the sectoral emission targets may mandate eligible entities, potentially the SEZ, to develop carbon budgets within which they must operate or face penalties. The new South African legislative framework will also carry cost-risks for the SEZ. The carbon tax payable by the SEZ tenants will be based on activity data reported to the Department of Environmental Affairs on an annual basis. The activity data relates to the consumption of the fossil fuels used by the SEZ tenants in their stationary equipment.
71
72
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DEA, 2017c. Declaration of Greenhouse Gases as Priority Air Pollutants, s.l.: National Environmental Management: Air Quality Act, 2004. DEA, 2017d. National Greenhouse Gas Emission Reporting Regulations., s.l.: National Environmental Management: Air Quality Act, 2004.. The South African Carbon Tax Act No 15 of 2019 was signed and the Act gazetted on 23 May 2019 (Gazette No. 42483) and the law effective from 1 June 2019.
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The activities in the SEZ will also be liable to pay carbon tax. By 2030, the carbon tax rate will be R206/tCO2, as per escalation provided for in the carbon tax act. National Treasury has indicated a high likelihood that that the allowances currently in the carbon tax act will be removed by 2030. If this should happen and all industries are operational, then this will lead to a tax liability of approximately R7bn in 2030 alone and is likely to increase year on year. In terms of regulatory implications, indirect carbon tax implications will further increase operational costs for the SEZ with regards to carbon tax on diesel purchases which may be in the region of an additional ZAR 9c/litre. During the construction phase, the SEZ will require building materials such as cement and steel. The prices of these products may increase with the introduction of the Carbon Tax Act 15 of 2019. This could ultimately increase the cost of construction for the SEZ. Furthermore, the carbon tax could potentially have an impact on the price of electricity. National Treasury has however given a commitment that there will be no impact of carbon tax on the electricity tariff up to 2022. After 2022 the carbon tax impact could be in the order of 5 cents per kWh, increasing to a potential level of 12 cents per kWh by 2030. It is expected that increases in electricity costs will be passed on to consumers in the second phase carbon tax which will further increase the SEZ’s construction phase costs in the order of 5 cents per kWh, increasing to a potential level of 12 cents per kWh by 2030. Costs of electricity could therefore increase by just under ZAR 1 million per year between 2022-2030 and by ZAR 2.3 million per year from 2030. Lastly, finding 4 of Climate Policy Initiative on Understanding the impact of a low carbon transition on south Africa indicates ‘The current South African system of incentives for new capital investment favour some existing industries that are exposed to transition risk, rather than new sectors that may create more sustainable sources of jobs and economic growth. Currently planned investment decisions could add more than $25 billion to the country’s transition risk’ 74 . This indicates that investments into new assets such as infrastructure, mines and refineries could enhance the transitional risk faced by companies, investor and the government. This is particularly relevant if resultant lower future revenues under a 2˚C scenario are insufficient to cover the investment cost and losses. This highlight the sustainability of such investments over industries or assets which are more resilient to transitional risk or which benefit from a low carbon transition.
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M, Huxham, M, Anwar, D Nelson, 2019. Climate Policy Initiative. Understanding the impact of a low carbon transition on South Africa. ACPI Energy Finance Report. Viewed 18 June 2019 https://climatepolicyinitiative.org/publication/understanding-the-impact-of-a-low-carbon-transition-on-southafrica/
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6.7 Summary of climate change resilience assessment The potential impacts of the different scenarios on the SEZ are summarised from the above section into Table 19 below. Table 21: Potential impact analysis for the SEZ under RCP8.5. Risks
Rating
Comments
Core Operations – SEZ Heat stress
High Risk
Water Stress
High Risk
Average temperatures are predicted to raise by between 2.35 ˚C 2.69˚C by 2050 with an increase in the number of hot days (>35 ˚C) of between 17 – 57 hot days. The culmination of increased average temperatures and heat stress can result in a greater number of people at risk of heat-related medical conditions. A temperature increase of 1.5˚C by the year 2100 could lead to a 2.2% drop in working hours45. The SEZ is located within water stressed area that is currently experiencing issues of water scarcity and water quality. Climate change will exacerbate water issues in this area particularly with predicted increases in drought and rainfall variability. The SEZ has acknowledge these challenges and has envisage to source water from Zimbabwe to supplement water that is planned to be acquired from the Limpopo River. Climate change models predict under best and worst case scenarios that average annual rainfall will decrease in all catchments of which are to supply water the SEZ from Zimbabwe. This further highlights the water supply risks associated with the SEZ large water demand. Additionally, it has been noted by the Vhembe District Municipality that existing water resources are being polluted by poor land management, poor sewage systems and agricultural pesticides resulting in less usable water. These issues will be of greater concern should the SEZ abstract ground and surface water from local water resources and thereby further limiting the amount of usable water for the area.
98
Risks
Rating
Disaster Medium risks - Flash Risk Floods
Comments As indicated in Figure 10, there is a medium risk of flash flooding within the area of the SEZ with a high risk of flooding within the Makhado and Soutpansberg escarpment area. Figure 27 indicates the increase in disaster weather event in the past year. Flooding will additionally pose a risk by disrupting operations of the SEZ by impacting access to the site and may impact on the functionality of machinery. Furthermore, flooding will also bring with it safety concerns as well as a risk of structural damage to infrastructure
Disaster risks Drought
High - Risk
Figure 20 indicates that there is a large increase in drought tendencies predicted for the period 2035 -2064. Increased drought has been found to bring with it an increase in the frequency of strong winds which can carry veld fires and destroy habitats. Therefore, drought will not only be an operation risk from a water perspective but also an infrastructure and health risk for the SEZ through knock-on consequences such as veld fires.
High Risk
The SEZ tenants will be liable for reporting emissions as per the National Greenhouse Gas Emissions Reporting Regulations. Noncompliance with these regulations will carry penalties that will range from fines to criminal prosecutions. As the SEZ is a large emitter of GHG emissions ensuring compliance will be critical. In this event, the SEZ tenants will also be liable for carbon tax and therefore having cost impactions during the operational phase. Carbon tax could also increase the construction costs as the cost of resource materials may increase to compensate for carbon tax liability.
Regulatory obligations
Value Chain - SEZ Disrupted supply chain
High Risk
It is assumed that the electricity for the construction phase will be supplied by Eskom. In terms of climate change impacts, there are two key considerations with regards to electricity derived from Eskom: the first being water and the second being the regulatory implications of the proposed carbon tax on the power utility. Decreasing water availability and quality may negatively affect the SEZ’s direct operations as well as the upstream and downstream value chain. The risk of supply chain disruptions for the construction phase of this project is medium, as the project is situated within a mining area which has sufficient stock levels of construction materials. However, the increased probability of storms may however impact the SEZ in 99
Risks
Rating
Comments terms of employee safety, infrastructure safety, production delays and increased insurance costs. Drought conditions and their impacts on the core operations, value chain and broader network may be further exacerbated as the proposed SEZ falls within a water stressed area. Therefore, water scarcity issues for pose a tremendous threat to a facility which is heavily dependent on water for operations.
Regulatory obligations
High Risk
The second phase of the Carbon Tax is will include a linkage to the national sectoral emission targets being developed by government. Once finalised, the sectoral emission targets may mandate eligible entities, potentially the SEZ, to develop carbon budgets within which they must operate or face penalties. Indirect carbon tax implications will further increase operational costs for the SEZ with regards to carbon tax on diesel purchases for example. Furthermore, the decarbonisation of Eskom’s operations could potentially carry a pricing risk for electricity. The carbon tax could potentially have an impact on the price of electricity. It is expected that increases in electricity costs will be passed on to consumers in the second phase carbon tax which will further increase the SEZ’s construction phase costs.
Social and Environmental context – Musina and Makhado Local Municipalities Community vulnerability
High Risk
South Africa is particularly vulnerable to climate change because of its dependence on climate-sensitive economic sectors, high levels of poverty and the inter-related impacts of community health and service delivery challenges. How badly a person or group will be affected will depend not only on their exposure to the event, but also on their social vulnerability to change in climate – that is, how well they are able to cope with and respond to events like flash floods, drought and heatwaves as discussed in this report. Table 19Error! Reference source not found. indicates the key demographics and the social context for the Musina and Makhado Local Municipalities. Due to, poor service delivery, a high dependency ratio, insufficient social infrastructure, few people having received formal education and high levels of poverty and unemployment, the Musina and Makhado Local Municipality is considered highly vulnerable to the impacts of climate change.
100
Risks
Rating
Comments
Heat stress
High Risk
Health is highlighted as a priority area of intervention in the Limpopo province due to the high levels of vulnerability to climate change. Of particular concern is the increase in temperatures which will have multiple health impacts and implications. The health impacts of extreme heat range from direct heat stress and heat stroke, to exacerbations of pre-existing heart failure, and even an increased incidence of acute kidney injury from dehydration in vulnerable populations. Elderly people, children younger than 12 months and people of poor health are particularly sensitive to these changes. Considering that average temperatures and the number of hot days are expected to increase, there is a high heat risk for the Musina and Makhado Local Municipality. This is particularly concerning as the Municipality shows high levels of social vulnerability.
In-migration High Risk
As evident in Vhembe District Municipality’s Climate Change Vulnerability Assessment and Response Plan, climate change will impact the municipality’s Local Economic Development Strategy. With the municipal population growing further pressure will be placed on demand for services and the overall regional economic base. This is especially the case in the agriculture, industrial and mining sectors which have been identified as key economic focus areas for the district. As such, vulnerable communities will increasingly look to these industries for solutions and increasing social pressure on the SEZ’s social license to operate.
Water supply
Climate change is expected to exacerbate the water scarcity and quality problems currently being experience in the area through drought, reduced runoff, increased evaporation, and an increase in flood events which have all been predicted to occur more frequently as described above.
High Risk
Enhanced evaporation rates will further cause the deterioration of water quality due to increased salt concentrations in dams, wetlands and soil/plant systems. Increased drought means less water is available to dilute wastewater discharges and irrigation return-flows to rivers. This results in reduced water quality and associated downstream health risks to aquatic ecosystems. These concerns result in less water being available for irrigation and drinking purposes, which impact negatively on the livelihoods of communities, especially in rural areas.
101
Risks
Rating
Comments
Ecosystem vulnerability
High Risk
Common under each projection is that the climate envelope in Limpopo is likely to resemble a different biome in future (Figure 32). This means that the endemic biota of the biome could experience significant climate-related stresses. Increased frequency of veld fires associated with drought induced winds have shown to destroy entire habitats and threaten the biodiversity of these ecosystems. With predictions indicating that drought and the number of hot days are expected to increase this will remain a concern for the area. Furthermore, drought has been exasperated by the limited supply of ground and surface water in the District. This is not expected to reduce as the population of the municipalities are expected to grow along with the fact that there will be a greater water demand for domestic, agricultural, industrial and mining purposes.
Under RCP 4.5 average annual temperatures are expected to increase to between 2.01˚C - 2.55˚C for the area where the SEZ is located. This is slightly lower than under RCP 8.5. Due to the social context of the Musina and Makhado Local Municipality, the above ratings will not significantly change with regards to the risks on the social and environmental contexts under RCP4.5. With regards to the impacts on the SEZ, the environmental setting of the area in which the SEZ is located is water stressed, prone to droughts and surrounded by vulnerable communities with respect to climate change impacts. As change in climate is expected to exacerbate these conditions, increases in average annual temperature of between 2.01˚C - 2.55˚C under RCP 4.5 will have similar impacts as under RCP 8.5 which indicates an increase of between 2.35 ˚C - 2.69˚C. Therefore, under RCP 4.5 the risk ratings will not significantly change.
Climate Change and the Possibility of Stranded Assets The global economy is currently experiencing a ‘carbon bubble’. The term ‘carbon bubble’ refers to the high-levels of extractable fossil fuels left in the earth compared to the low-levels of fossil fuel emissions that the earth’s atmosphere can accommodate before catastrophic levels of climate change ensue. The carbon bubble concept is illustrated in the following Figure 33. The amount of coal in the global reserves accounts for 1,500-2,000 gigatons of CO2e, whereas the amount of emissions that could still be emitted before reaching the 2⁰C limit is less than 1,000 gigatons of CO2e.
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Figure 33: Comparison of the global 2°C carbon budget with fossil fuel reserves CO2 emissions potential75. Current plans by governments to mitigate global greenhouse gas levels to levels that limit a 2⁰C increase in global temperatures (compared to pre-industrial levels) are insufficient. The shortfall in country-level Intended Nationally Determined Contributions (precursors to the NDCs submitted under the Paris Agreement) is illustrated in the following Figure 34.
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Leaton, J., 2011. Carbon bubble growing but markets aren’t listening. Viewed 25 July 2019 https://www.greenbiz.com/blog/2011/07/15/carbon-bubble-growing-markets-arent-listening
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Figure 34: Shortfall in country level contributions to meet the 2⁰C target76. The Paris Agreement takes cognisance of the initial shortfall in ambitions and provides for a ratcheting mechanism in which countries can increase the level of ambition of the NDCs. The ratcheting mechanism includes: 2015
Countries submitted their NDCs
2018
Countries took stock of collective efforts in relation to the long-term goal of the Paris Agreement. This stocktake will inform the preparation of the next round of pledges.
2020
Countries with 2025 targets to communicate their second round of climate pledges, while countries with 2030 targets will communicate or update their pledge. New climate pledges will then be submitted every five years.
2023
Global stocktake on mitigation, adaptation and finance.
2025
Countries to submit their third round of climate pledges
2028
Second global stocktake
The implication of the ratcheting mechanism is that countries that are party to the Paris Agreement (such as South Africa) will be increasing national targets to reduce greenhouse gas emissions over the next decade. National targets could increase pressures or penalties on emission intensive
76
UNFCCC, 2016. Aggregate effect of the intended nationally determined contributions: an update, s.l.: United Nations.
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businesses to limit greenhouse gas emissions, such as coal fire power stations and steel producers, both of which are proposed to be built within the SEZ. The competitiveness of fossil fuel industries may be further threatened by cost reductions in renewable energies, particularly solar and wind. For example, between 2010-2017 the costs of onshore wind power fell by around 23% and solar photovoltaic electricity fell by 73% (Figure 35).
Figure 35: Global levelized cost of electricity from utility-scale renewable power generation technologies, 2010-201777. It is expected that, by 2020, the renewable power generation technologies that are now in commercial use will fall within the fossil fuel-fired cost range. In most cases renewable energy will be cheaper than fossil fuels77. The proposed coal fired power plant at the SEZ may therefore be at risk of becoming a stranded asset considering the likelihood of the legal and commercial pressures related to increased national emission reduction targets and increased number of competitors in the energy space.
Mitigation and Adaptation 8.1 Design considerations Due to the lack of data provided by the client and project developer (as described in Sections 4.1 and 5) detailed mitigation measures could not be determined.
77
IRENA, 2018. Renewable power generation costs in 2017, s.l.: IRENA.
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The majority of the SEZ emissions will occur during the operational phase. Therefore, emission mitigation measures would need to be focused on this phase to be effective in reducing the impacts the SEZ will have on climate change. Climate change mitigation is generally centred round four main strategies: 1. Using renewable energies; 2. Using new, more efficient technologies; 3. Retrofitting older equipment to be more energy efficient; and 4. Changing management practices or consumer behaviour to be more emissions conscious. For the various planned operations in the SEZ, mitigation would be focused on two main aspects, energy efficient technologies and the use of renewable energies. Energy efficient technologies can assist in reducing the total amount of electricity required in the first place, reducing the Scope 2 emissions irrespective of the electricity source. It could also assist in reducing Scope 1 emissions. Further, if the various SEZ operations switch to using more renewable energy sources, such as solar and/or wind, it could reduce its energy related emissions even further. A detailed assessment on the potential use of renewable energy for the various planned operations of the SEZ would be required during the assessment of the individual operations. The mitigated emissions scenario is supported by the Paris Agreement and will be achieved as countries set ambitious NDCs (Nationally Determined Contributions). As countries work towards compiling their NDCs, additional regulations may be put in place to limit emissions from fossil fuel intensive industries or encourage renewable energy development. Evidence of this scenario were evident at the 24th Conference of the Parties (COP 24) held in Katowice, Poland in December 2018. The main issue under consideration at this event was global shortfall in targets to reach the goal of limiting average temperatures below 2°C above pre-industrial levels. In this regard countries must negotiate and determine how to achieve such a target, and how to possibly accelerate efforts to achieve a 1.5°C target through a ratchet mechanism. The ratchet mechanism requires countries to submit new NDCs every five years, outlining how much they intend to increase ambition, and reduce emissions. Each submission should be more ambitious than the last. South Africa’s NDC has been assessed as insufficient to meet a 2°C target. A ratcheted South African NDC (which could be categorised as a transitional risk) within the approximate period 2022-2025 could have an impact on the longevity of projects such as the proposed SEZ.
8.2 Operational Emissions Management South Africa’s environmental legal framework provides for the mandatory management of emissions by the owners of entities that have operational control over emissions-intensive activities. The National Pollution Prevention Plans Regulations and the National Greenhouse Gas Emission Reporting Regulations refer.
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Projects implemented in the SEZ will be required to develop a pollution prevention plan, as there are a number of listed production process in the National Pollution Prevention Plans Regulations published under the National Environmental Management Act: Air Quality which are applicable to the SEZ such as the production of iron, steel, ferro-alloys and electricity from fossil fuels. The National Greenhouse Gas Emission Reporting Regulations require entities that are above the defined thresholds to report direct (Scope 1) emissions only, excluding road and off-road transport. This is particularly relevant to the production of iron, steel, ferro-alloys and electricity from fossil fuels, which will need to be reported to Department of Environmental Affairs. In this instance, such facilities would need to monitor and report their annual (calendar year) emissions associated with the combustion of fossil fuels in the stationary equipment. Entities within the MMSEZ could use carbon credits purchased from established carbon markets to offset some of the emissions generated. Although this does not reduce direct emissions from the MMSEZ itself, this can help reduce the impact of the MMSEZ on a global scale. This would come at a considerable cost to the MMSEZ. Assuming an average cost of approximately €30/t78, and that all emissions are to be offset, this approach would cost the MMSEZ approximately €1bn per year once fully operational.
Opinion on the Project When considered from a South African National perspective, the impacts of the project are: The project has a High (negative) impact rating for the operational phase of the project, in terms of the 2014 NEMA EIA Regulations, with a significance score of 100. The emissions released by the various activities associated with the SEZ over the operational lifetime of the project will consume as much as 10% of South Africa’s carbon budget. The impact on the emission inventory of the country is therefore VERY HIGH (negative). When considering the impact score for the construction phase, the impact score will be High. This is independent of the magnitude of the GHG emissions. However, these emissions pale in comparison to the operational emissions that will result from the proposed SEZ and various activities planned within. Although the impact of the activities associated with operational phase of the SEZ is considered to be HIGH with a magnitude impact (in terms of the specialist climate change assessment methodology) of VERY HIGH in terms of the country’s emission inventory, such impact has been considered within the context of the provisions of the Thabametsi case, as well as the relevant
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Nina Chestney. 2021. Europe carbon prices expected to rise to 2030-industry survey. Reuters. Available at https://www.reuters.com/business/sustainable-business/europe-carbon-prices-expected-rise-2030-industrysurvey-2021-06-14/
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regulatory requirements relating to South Africa’s energy sector, climate change commitments and social context. • The contextual consideration of the project aligns with the requirements of Section 240(1) of NEMA which provides that the Minister must comply with the Act, and must “take into account all relevant factors.” At the time of drafting the report, the IRP 2010-2030 was the binding policy determining South Africa’s electricity mix. • However, since the adoption of the IRP 2010, South Africa has made numerous climate change commitments in its NDC, and as such, the IRP 2010 is premised on facts that are outdated when considering more recent policy developments and commitments. Therefore, environmental authorisation of the thermal coal fired power plant cannot be granted merely based on the fact that the IRP 2010 allows for energy to be procured from coal. Additional factors such as the project’s overall impact in relation to other factors such as South Africa’s NDC and South Africa’s Peak Plateau Decline (PPD) emission trajectory must be considered. Based on the above, and considering the relevant regulatory factors which includes, but is not limited to South Africa’s Nationally Determined Contribution (NDC), the Peak Plateau Decline (PPD) emission trajectory as well as the outdated nature of the Integrated Resource Plan 2010, the various activities planned as part of the SEZ should not be implemented, unless the following can be met: • If the individual processes within the SEZ are built according to the SBTi intensities identified in the report (see Table 14), then emissions of the project could be reduced by approximately 10 million tonnes per year, to a total emissions of 24 million tonnes per year. In the light of the above, our recommendations for the project are: • Environmental authorisations for the individual plants in the SEZ should only be granted if the following emission intensities can be achieved: Plant Coke Plant Ferrochrome plant Ferromanganese plant Silicon-manganese plant Carbon steel plant Stainless steel plant Lime plant Cement plant Sewage treatment plant Water treatment plant
2°C target intensities for 2030
0.21 tCO2e/tonne product 3.37 tCO2e/tonne product 3.37 tCO2e/tonne product 5.18 tCO2e/tonne product 0.37 tCO2e/tonne product 0.78 tCO2e/tonne product 0.87 tCO2e/tonne product 0.80 tCO2e/tonne clinker 0.0005 tCO2e/tonne water 0.0005 tCO2e/tonne water
In addition, the environmental authorisation should require a re-assessment of the emission intensities 5 years after the start of operation of the respective plants 108
The construction of a coal fired thermal power plant should not be approved unless the plant is fitted with a carbon capture and storage unit that can sequester ALL emissions from the combustion of coal from the starting date of operation. Without CCS, the coal fired power station will severely reduce South Africa’s ability to achieve its NDC. We make this recommendation in the context of the comment regarding the feasibility of CCS as described in Section 4.1.3. In practical terms this means that approval for the coal fired thermal power plant should, in our opinion, not be granted. Water is of critical concern. The study area is already severely water stressed and climatic modelling for the area indicates increased ambient temperatures, prolonged periods of drought and greater rainfall variability. These factors will exacerbate current water risks, both in South Africa and in neighbouring Zimbabwe. The impacts of climate change, as well as the potential changes in climatic parameters have, a broader impact on water sources than the immediate zone of influence. Current water stress in the region is anticipated to be exacerbated by climate change impacts. The area is anticipated to become increasingly hotter and drier, thus the water availability in the area may critically constrained resulting in water shortages affecting the region in its entirety. We are thus of the opinion that any approval of the project should be conditional upon climate change and detailed climate change modelling being considered in the ground water and surface water studies done for the project. In addition, we suggest that any approval of the project should be conditional upon an overall water risk analysis of the region (Limpopo Province) being conducted, with specific reference to the proposed SEZ project. This is to identify the broader water stress and possible pollution risks posed by the proposed SEZ, which will be exacerbated by the impacts of climate change in the Province. It is advised that a regional perspective be developed with regards to water resources in the Province, current land use change patterns, existing water uses and climate change. This will allow for more informed decision-making related to the development of the proposed SEZ. Furthermore, the provision of water will rely on an international supply of water from Zimbabwe which is also predicted to experience increases in water stress as climate change progresses. Thus, any approval of the project should be conditional upon a thorough assessment of how the diversion of this water will impact the climate change-related adaptive capacity of the affected communities in Zimbabwe. Elevated temperatures, specifically an increase in very hot days, will increase the risk of employees suffering from heat-related illnesses. To prevent this, all indoor working environments should be well insulated and air conditioned and drinking water should be made readily available throughout the MMSEZ. This is to minimise the potential impacts of heat-related health impacts, such as dehydration, on the health of employees.
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The Vhembe District Municipality has a highly vulnerable population in terms of climate change. This population is characterised by high levels of unemployment and low levels of education. In addition, there are significant service delivery backlogs within the area. Climate change could worsen the socio-economic conditions of these communities, as could an increased influx of people to this area as a result of this proposed project. In addition, due to the location and scale of the SEZ, and given the vulnerability of communities in Zimbabwe and Mozambique, the study area could see an increase in migratory job-seekers. This will further compound social pressures. The potential impacts of climate change in this area, within the context of this project, such as increasing temperatures, prolonged periods of drought, increased frequency of flash flooding, biodiversity and agricultural loss and significant water related constraints, could have significant impacts on the project itself as well as entrench the vulnerability of people in the area. This will increase poverty and prevent communities from building climate resilience, specifically in the longterm.
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