Climate change and extreme weather events can significantly impact energy infrastructure in three main ways:
1. Extraction and resources are threatened by rising sea levels, melting permafrost, and flooding which can damage offshore oil/gas rigs, mines, and disrupt supply chains.
2. Conversion processes from different sources like thermal, nuclear, and hydro face efficiency losses from higher temperatures, drought, and flooding which can force shutdowns.
3. Transmission and distribution networks are vulnerable to weather damage from high winds, flooding, lightning, and overheating which causes blackouts.
The economic costs of not adapting energy systems to these impacts include physical damage, lost output, higher prices, and macroeconomic losses
This document summarizes the latest climate science from the Met Office and its implications for Wales. It discusses increasing global temperatures, rising carbon dioxide levels, extreme weather events, and projections showing continued warming if emissions are not reduced. Climate models are improving but still have uncertainties around factors like ocean heat uptake. The impacts of 4°C warming could include drought, flooding, reduced crops, and effects on billions of people. Improving model resolution helps understand regional implications like for Welsh terrain and rainfall.
Climate change and Architects role and resposibilitiesShereen Khashaba
Engineers and architects can play a role in addressing climate change through their design and construction of more sustainable buildings. Reducing fossil fuel usage and greenhouse gas emissions from the building sector is key as it is currently the largest contributor to carbon dioxide emissions in the US. Targets need to be set to reduce energy consumption from new and renovated buildings by at least 50% compared to current levels by 2030 through sustainable design and use of renewable energy. Aggressive implementation of more stringent building codes that meet these targets can significantly cut CO2 emissions and help address the climate crisis.
On June 14, 2019 ICLR conducted a Friday Forum webinar led by Dr. Nathan Gillett and Dr. Xuebin Zhang. This report is about how and why Canada’s climate has changed and what changes are projected for the future. Led by Environment and Climate Change Canada, this document is the first of a series to be released as part of Canada in a Changing Climate: Advancing our Knowledge for Action. It documents changes across Canada in temperature, precipitation, snow, ice, and permafrost, freshwater availability as well as in Canada’s three oceans. It can be viewed at www.changingclimate.ca/CCCR2019
Dr. Nathan Gillett is a Research Scientist at the Canadian Centre for Climate Modelling and Analysis in Environment and Climate Change Canada’s Climate Research Division. His research is focused on understanding and attribution of climate change. He is a Coordinating Lead Author of the chapter “Human influence on the climate system” of the upcoming IPCC Working Group I Sixth Assessment Report, and he served as a Lead Author of the IPCC Fourth and Fifth Assessment Reports. Dr. Gillett has a PhD in atmospheric physics from the University of Oxford.
Dr. Xuebin Zhang is a senior research scientist with Environment and Climate Change Canada’s Climate Research Division. His main research focus is past and future changes in weather and climate extremes. He was a lead author for the IPCC Special Report on Managing the Risks of Extreme Events and Disasters to Advance Climate Change Adaptation and IPCC Working Group I Fifth Assessment Report. He is a Coordinating Lead Author of the climate extremes chapter in the IPCC Working Group I Sixth Assessment Report. Dr. Zhang has a background in engineering hydrology. He received a PhD degree in Physics (Climatology) from University of Lisbon, Portugal.
The document discusses how to build adaptive capacity to climate change in the UK. It provides an overview of the UK Climate Impacts Programme (UKCIP) which aims to help organizations adapt to climate change impacts through research partnerships and capacity building programs. It summarizes projections from UK Climate Projections including higher temperatures, more extreme weather events, and sea level rise. It also outlines impacts to consider for business and infrastructure planning like disruption from flooding and heat waves.
Projected climate change impacts in sundarbansWWF-India
1) The document discusses projected impacts of climate change on the Sundarbans region, including rising sea levels, increased temperatures, changes in rainfall patterns, and increased intensity of tropical cyclones.
2) Models project that the Sundarbans will experience significant inundation and land loss due to sea level rise, which will be exacerbated by sinking of the delta and tilting of the Bengal Basin. This poses major threats to the ecology and human populations in the region.
3) Climate change is also expected to negatively impact agriculture and water availability in the Sundarbans, endanger plant and animal species found only in the region, and increase risks from natural disasters like flooding from tropical cyclones and storm surge
The document discusses the relationship between greenhouse gas emissions, climate change, and global warming based on scientific data and models. It summarizes that carbon emissions can reliably predict increases in atmospheric CO2 levels, which can then be used to model radiative forcing and projected temperature increases. Feedback loops may accelerate warming beyond current predictions. The Arctic and Greenland are already experiencing significant impacts like sea ice loss and melting.
The document discusses the greenhouse effect and how it leads to warming of the Earth. It explains that greenhouse gases like carbon dioxide and methane trap heat in the atmosphere and have increased due to human emissions. Data from ice cores shows a clear correlation between CO2 levels, temperature, and sea level rise over hundreds of thousands of years. While CO2 levels have increased about 40% since the industrial revolution, emissions continue to rise rapidly and could lead to over 2 degrees Celsius of warming with serious consequences if left unchecked.
This document summarizes the latest climate science from the Met Office and its implications for Wales. It discusses increasing global temperatures, rising carbon dioxide levels, extreme weather events, and projections showing continued warming if emissions are not reduced. Climate models are improving but still have uncertainties around factors like ocean heat uptake. The impacts of 4°C warming could include drought, flooding, reduced crops, and effects on billions of people. Improving model resolution helps understand regional implications like for Welsh terrain and rainfall.
Climate change and Architects role and resposibilitiesShereen Khashaba
Engineers and architects can play a role in addressing climate change through their design and construction of more sustainable buildings. Reducing fossil fuel usage and greenhouse gas emissions from the building sector is key as it is currently the largest contributor to carbon dioxide emissions in the US. Targets need to be set to reduce energy consumption from new and renovated buildings by at least 50% compared to current levels by 2030 through sustainable design and use of renewable energy. Aggressive implementation of more stringent building codes that meet these targets can significantly cut CO2 emissions and help address the climate crisis.
On June 14, 2019 ICLR conducted a Friday Forum webinar led by Dr. Nathan Gillett and Dr. Xuebin Zhang. This report is about how and why Canada’s climate has changed and what changes are projected for the future. Led by Environment and Climate Change Canada, this document is the first of a series to be released as part of Canada in a Changing Climate: Advancing our Knowledge for Action. It documents changes across Canada in temperature, precipitation, snow, ice, and permafrost, freshwater availability as well as in Canada’s three oceans. It can be viewed at www.changingclimate.ca/CCCR2019
Dr. Nathan Gillett is a Research Scientist at the Canadian Centre for Climate Modelling and Analysis in Environment and Climate Change Canada’s Climate Research Division. His research is focused on understanding and attribution of climate change. He is a Coordinating Lead Author of the chapter “Human influence on the climate system” of the upcoming IPCC Working Group I Sixth Assessment Report, and he served as a Lead Author of the IPCC Fourth and Fifth Assessment Reports. Dr. Gillett has a PhD in atmospheric physics from the University of Oxford.
Dr. Xuebin Zhang is a senior research scientist with Environment and Climate Change Canada’s Climate Research Division. His main research focus is past and future changes in weather and climate extremes. He was a lead author for the IPCC Special Report on Managing the Risks of Extreme Events and Disasters to Advance Climate Change Adaptation and IPCC Working Group I Fifth Assessment Report. He is a Coordinating Lead Author of the climate extremes chapter in the IPCC Working Group I Sixth Assessment Report. Dr. Zhang has a background in engineering hydrology. He received a PhD degree in Physics (Climatology) from University of Lisbon, Portugal.
The document discusses how to build adaptive capacity to climate change in the UK. It provides an overview of the UK Climate Impacts Programme (UKCIP) which aims to help organizations adapt to climate change impacts through research partnerships and capacity building programs. It summarizes projections from UK Climate Projections including higher temperatures, more extreme weather events, and sea level rise. It also outlines impacts to consider for business and infrastructure planning like disruption from flooding and heat waves.
Projected climate change impacts in sundarbansWWF-India
1) The document discusses projected impacts of climate change on the Sundarbans region, including rising sea levels, increased temperatures, changes in rainfall patterns, and increased intensity of tropical cyclones.
2) Models project that the Sundarbans will experience significant inundation and land loss due to sea level rise, which will be exacerbated by sinking of the delta and tilting of the Bengal Basin. This poses major threats to the ecology and human populations in the region.
3) Climate change is also expected to negatively impact agriculture and water availability in the Sundarbans, endanger plant and animal species found only in the region, and increase risks from natural disasters like flooding from tropical cyclones and storm surge
The document discusses the relationship between greenhouse gas emissions, climate change, and global warming based on scientific data and models. It summarizes that carbon emissions can reliably predict increases in atmospheric CO2 levels, which can then be used to model radiative forcing and projected temperature increases. Feedback loops may accelerate warming beyond current predictions. The Arctic and Greenland are already experiencing significant impacts like sea ice loss and melting.
The document discusses the greenhouse effect and how it leads to warming of the Earth. It explains that greenhouse gases like carbon dioxide and methane trap heat in the atmosphere and have increased due to human emissions. Data from ice cores shows a clear correlation between CO2 levels, temperature, and sea level rise over hundreds of thousands of years. While CO2 levels have increased about 40% since the industrial revolution, emissions continue to rise rapidly and could lead to over 2 degrees Celsius of warming with serious consequences if left unchecked.
This document summarizes key points from a course on climate change:
1. We are already experiencing impacts from 0.6-0.8°C of warming and have at least another 0.6-0.8°C committed due to past emissions.
2. Continuing at current emission rates would take us to 450ppm CO2 by 2035, a potential "tipping point" for climate change and ecosystems.
3. Warming of 2°C may be too much and could lead to further warming from feedbacks like melting ice sheets and methane release potentially taking us to 3°C.
1) Climate change consequences like storms, droughts and heat waves are already occurring at just 0.8°C of warming.
2) Carbon dioxide levels are on a trajectory to hit 450 ppm by 2030-2035, committing us to around 2°C of warming and severe ocean acidification.
3) Amplifying feedbacks like ice sheet melting, methane releases and reduced Arctic albedo could push warming above 2°C to 3°C or more, levels that may have uncontrollable impacts on the biosphere.
The document summarizes evidence that the climate is changing faster than usual due to human activities. It discusses how scientists have measured increasing levels of CO2 and other greenhouse gases in the atmosphere since the Industrial Revolution. Measurements from Mauna Loa Observatory since 1957 show that CO2 levels have increased by 1.5-2.5% per year. The Intergovernmental Panel on Climate Change's Fourth Assessment Report in 2007 represented an overwhelming scientific consensus that climate change poses a serious risk and is at least 90% certain to be caused by human activity like burning fossil fuels. The report projected impacts of climate change like rising sea levels, stronger storms, and heat waves.
Are ‘little ice ages’ and ‘megadroughts’ possible?
Scientists are investigating whether changes in ocean circu- lation may have played a role in causing or amplifying the “Little Ice Age” between 1300 and 1850. This period of abruptly shift- ing climate regimes and more severe winters had profound agri- cultural, economic, and political impacts in Europe and North America and changed the course of history.
Conclusions
Ocean Mixed Layer Temperatures for both models are very similar, showing that the ocean conditions for the LGM and future climate underwent the same conditions at some point, could lead to colder temperatures
With this data alone available, we must infer that there could be a climate change due to melting of ice into the ocean, until there is more data to back up the hypothesis
EdGCM limits the amount of information we can compare
○ Only 100 years of predicted models
○ Not as many parameters available to model
Climate Change Basics: Issues and Impacts for BoatingNASBLA
State Climatologist David Zierden presented Climate Change Basics: Issues and Impacts for Boating to the National Association of State Boating Law Administrators on September 9, 2008
This document provides an overview of climate change, including definitions, evidence, causes, impacts, and ways to control it. It begins by defining climate change and distinguishing it from weather change. It then outlines various physical evidence of climate change, such as rising global temperatures and sea levels. Major causes of climate change discussed include greenhouse gas emissions from human activities like burning fossil fuels. Impacts described are more extreme weather, rising seas, species extinction, and effects on countries like Pakistan. The document concludes by discussing approaches to address climate change through mitigation, adaptation, and climate engineering.
Climate Change Seal Level Rise Met OfficeMr Cornish
The document discusses evidence that the Earth's climate is warming due to human activities. It notes that global temperatures and sea levels have increased over the past century, precipitation patterns have changed, and glaciers are retreating. The document projects that these trends will continue in the future, causing more warming, sea level rise, and extreme weather if emissions are not reduced. Coastal areas and developing nations will be most vulnerable to the impacts of climate change.
The Bidani House project demonstrates how to design a climate-responsive building on a constrained urban site. Located in Faridabad's composite climate zone, the house has large temperature swings throughout the year. Key sustainable features include developing the house form around a central courtyard to act as a heat sink, using buffer spaces on the overheated southwestern exposure, allowing solar penetration according to seasonal changes through the building form, and using local stone for thermal mass to moderate temperature swings. The project shows how responsive design is possible even on a fixed small urban site.
The document summarizes the key findings from IPCC reports on the likely impacts of climate change. It discusses that global surface temperatures are projected to increase 1.1-6.4°C by 2100, higher than any warming seen in the last 650,000 years. Precipitation patterns will be disrupted and extreme weather events will increase in severity and frequency. Sea levels are projected to rise 18-59 cm by 2100 but could be higher depending on ice sheet melting. Some climate changes such as ocean warming and sea level rise will continue for centuries.
The EXPLODING POPULATION OF 7 B IS INFLUENCING OUR CLIMATE BY BURNING FOSSIL FUELS THAT EMIT CARBON DIOXIDE, CO2.
1. THE HUMAN INFLUENCE ON WARMING
Emissions of the greenhouse gas CO2 are increasing at a rate of 2.5 ppm per year.
2. CONTRAST THIS WITH SLOWER NATURAL PROCESSES
18K – 10K years ago, C02 increased at a rate 1/300th slower.
3. THE IMPACT OF CONTINUING CLIMATE CHANGE
Melting of the Arctic is increasing our winter climate extremes.
This document discusses climatic conditions and building strategies in different climate zones of India. It begins by defining weather and climate, then lists six factors that affect climate. It describes five different climate types found in India - hot and dry, warm and humid, moderate, cold and cloudy, and cold and sunny - providing examples of locations and details on temperature, humidity, and precipitation for each. It concludes by outlining implications for building design strategies in each climate zone.
This document summarizes several effects of global warming seen in Italy, including melting glaciers and permafrost, increasing heat waves, rising sea levels, coastal erosion, more frequent floods, and cyclones in the Mediterranean region. Glacial melting is caused by global warming and less albedo and can lead to flooding, landslides, and loss of hydroelectric power. Permafrost melting releases greenhouse gases and causes rockfalls. Analysis shows heat waves in Italy are becoming more intense, frequent, and longer due to global warming. Rising sea levels flood lands and cause coastal erosion, threatening beaches. Floods and mountain cloudbursts also cause more destruction.
A microclimate is a local climate that differs from the area around it. Several factors can impact microclimates, including vegetation like hedges and trees, physical features such as bodies of water, the aspect or direction a surface faces, and human-made structures. These factors can cause areas to be warmer or cooler through mechanisms like shading, wind blocking, and heat absorption and reflection.
This document discusses various natural and human factors that can influence climate change. It describes several natural processes such as volcanic eruptions, ocean circulation patterns, solar activity, and Earth's orbital and rotational changes that have short or long-term effects on climate. It also explains how human activities like burning fossil fuels and deforestation have increased greenhouse gases in the atmosphere and led to issues like global warming and ocean acidification. The document provides examples and diagrams to illustrate these concepts and their impacts on climate.
The document summarizes key findings from the IPCC's Fifth Assessment Report regarding climate change projections for South Asia. It finds that human activity is the dominant cause of warming since the 1950s. If emissions continue at a high rate, the Arctic Ocean will likely be ice-free in summers by 2050. South Asia will experience increased temperatures, rainfall, and sea level rise by mid-century, posing challenges for coastal areas, agriculture, and infrastructure. Adaptation and mitigation efforts are needed to reduce impacts.
1) Global warming is caused by increased levels of greenhouse gases like carbon dioxide trapping heat in the lower atmosphere. The thin layer of atmosphere where climate occurs can be influenced by human activity.
2) Human activities like burning fossil fuels have increased atmospheric CO2 levels by about 30% since the industrial revolution, contributing to observed rising global temperatures according to computer models.
3) Potential impacts of unmitigated climate change include rising sea levels, worsening extreme weather, melting ice caps and glaciers, and damage to ecosystems. Reducing emissions from coal power plants, increasing renewable energy and energy efficiency can help address the problem.
The document discusses differences in climate between northern and southern Africa, which are divided by the equator. The northern part includes the Sahara desert, while the southern part includes grasslands. Climate varies in different regions due to geography, with tropical climates near the equator and colder climates farther north and south. Additional factors like altitude, prevailing winds, and distance from the sea also impact regional climates. The document then covers various climate types, weather phenomena, factors influencing climate, and seasonal changes caused by the earth's axial tilt.
The Arctic ecosystem that sustains Arctic residents is melting as temperatures rise, melting permafrost and draining inland freshwater into the ocean. Global warming is increasing temperatures by 3 to 5°C by 2100, rising sea levels by 25 meters, eliminating the Arctic ice cap, and potentially completely melting the Greenland glacier. Increased risks of infectious diseases like malaria, dengue fever, yellow fever, and more frequent cholera outbreaks may also occur due to climate change effects like warmer temperatures.
The document summarizes several effects of climate change that have already been observed and are projected to continue or worsen in the future. Key effects mentioned include rising sea levels and melting polar ice caps destroying animal habitats; longer frost-free seasons and growing seasons affecting ecosystems and agriculture; more frequent and intense heat waves, droughts, and hurricanes; and projections that the Arctic ocean could become ice-free in summer before mid-century while sea levels are expected to rise 1-4 feet by 2100.
Spatio-temporal analyses of the impacts of extreme weather events on renewabl...Global Risk Forum GRFDavos
This document discusses the impacts of extreme weather events on renewable energy infrastructure in Germany. It outlines that heavy rain can damage hydroelectric plants and reduce output. Wind turbines are vulnerable to tornadoes and severe storms. Photovoltaic panels can be disturbed by thunderstorms, hail, high winds and lightning. Germany's climate mitigation concepts aim to integrate risk analyses of extreme weather with analyses of potential renewable energy sites. Regulations for distances between infrastructure and weather risks could be standardized nationwide. The concepts seek to develop sustainable renewable energy systems resilient to climate change impacts.
This document summarizes key points from a course on climate change:
1. We are already experiencing impacts from 0.6-0.8°C of warming and have at least another 0.6-0.8°C committed due to past emissions.
2. Continuing at current emission rates would take us to 450ppm CO2 by 2035, a potential "tipping point" for climate change and ecosystems.
3. Warming of 2°C may be too much and could lead to further warming from feedbacks like melting ice sheets and methane release potentially taking us to 3°C.
1) Climate change consequences like storms, droughts and heat waves are already occurring at just 0.8°C of warming.
2) Carbon dioxide levels are on a trajectory to hit 450 ppm by 2030-2035, committing us to around 2°C of warming and severe ocean acidification.
3) Amplifying feedbacks like ice sheet melting, methane releases and reduced Arctic albedo could push warming above 2°C to 3°C or more, levels that may have uncontrollable impacts on the biosphere.
The document summarizes evidence that the climate is changing faster than usual due to human activities. It discusses how scientists have measured increasing levels of CO2 and other greenhouse gases in the atmosphere since the Industrial Revolution. Measurements from Mauna Loa Observatory since 1957 show that CO2 levels have increased by 1.5-2.5% per year. The Intergovernmental Panel on Climate Change's Fourth Assessment Report in 2007 represented an overwhelming scientific consensus that climate change poses a serious risk and is at least 90% certain to be caused by human activity like burning fossil fuels. The report projected impacts of climate change like rising sea levels, stronger storms, and heat waves.
Are ‘little ice ages’ and ‘megadroughts’ possible?
Scientists are investigating whether changes in ocean circu- lation may have played a role in causing or amplifying the “Little Ice Age” between 1300 and 1850. This period of abruptly shift- ing climate regimes and more severe winters had profound agri- cultural, economic, and political impacts in Europe and North America and changed the course of history.
Conclusions
Ocean Mixed Layer Temperatures for both models are very similar, showing that the ocean conditions for the LGM and future climate underwent the same conditions at some point, could lead to colder temperatures
With this data alone available, we must infer that there could be a climate change due to melting of ice into the ocean, until there is more data to back up the hypothesis
EdGCM limits the amount of information we can compare
○ Only 100 years of predicted models
○ Not as many parameters available to model
Climate Change Basics: Issues and Impacts for BoatingNASBLA
State Climatologist David Zierden presented Climate Change Basics: Issues and Impacts for Boating to the National Association of State Boating Law Administrators on September 9, 2008
This document provides an overview of climate change, including definitions, evidence, causes, impacts, and ways to control it. It begins by defining climate change and distinguishing it from weather change. It then outlines various physical evidence of climate change, such as rising global temperatures and sea levels. Major causes of climate change discussed include greenhouse gas emissions from human activities like burning fossil fuels. Impacts described are more extreme weather, rising seas, species extinction, and effects on countries like Pakistan. The document concludes by discussing approaches to address climate change through mitigation, adaptation, and climate engineering.
Climate Change Seal Level Rise Met OfficeMr Cornish
The document discusses evidence that the Earth's climate is warming due to human activities. It notes that global temperatures and sea levels have increased over the past century, precipitation patterns have changed, and glaciers are retreating. The document projects that these trends will continue in the future, causing more warming, sea level rise, and extreme weather if emissions are not reduced. Coastal areas and developing nations will be most vulnerable to the impacts of climate change.
The Bidani House project demonstrates how to design a climate-responsive building on a constrained urban site. Located in Faridabad's composite climate zone, the house has large temperature swings throughout the year. Key sustainable features include developing the house form around a central courtyard to act as a heat sink, using buffer spaces on the overheated southwestern exposure, allowing solar penetration according to seasonal changes through the building form, and using local stone for thermal mass to moderate temperature swings. The project shows how responsive design is possible even on a fixed small urban site.
The document summarizes the key findings from IPCC reports on the likely impacts of climate change. It discusses that global surface temperatures are projected to increase 1.1-6.4°C by 2100, higher than any warming seen in the last 650,000 years. Precipitation patterns will be disrupted and extreme weather events will increase in severity and frequency. Sea levels are projected to rise 18-59 cm by 2100 but could be higher depending on ice sheet melting. Some climate changes such as ocean warming and sea level rise will continue for centuries.
The EXPLODING POPULATION OF 7 B IS INFLUENCING OUR CLIMATE BY BURNING FOSSIL FUELS THAT EMIT CARBON DIOXIDE, CO2.
1. THE HUMAN INFLUENCE ON WARMING
Emissions of the greenhouse gas CO2 are increasing at a rate of 2.5 ppm per year.
2. CONTRAST THIS WITH SLOWER NATURAL PROCESSES
18K – 10K years ago, C02 increased at a rate 1/300th slower.
3. THE IMPACT OF CONTINUING CLIMATE CHANGE
Melting of the Arctic is increasing our winter climate extremes.
This document discusses climatic conditions and building strategies in different climate zones of India. It begins by defining weather and climate, then lists six factors that affect climate. It describes five different climate types found in India - hot and dry, warm and humid, moderate, cold and cloudy, and cold and sunny - providing examples of locations and details on temperature, humidity, and precipitation for each. It concludes by outlining implications for building design strategies in each climate zone.
This document summarizes several effects of global warming seen in Italy, including melting glaciers and permafrost, increasing heat waves, rising sea levels, coastal erosion, more frequent floods, and cyclones in the Mediterranean region. Glacial melting is caused by global warming and less albedo and can lead to flooding, landslides, and loss of hydroelectric power. Permafrost melting releases greenhouse gases and causes rockfalls. Analysis shows heat waves in Italy are becoming more intense, frequent, and longer due to global warming. Rising sea levels flood lands and cause coastal erosion, threatening beaches. Floods and mountain cloudbursts also cause more destruction.
A microclimate is a local climate that differs from the area around it. Several factors can impact microclimates, including vegetation like hedges and trees, physical features such as bodies of water, the aspect or direction a surface faces, and human-made structures. These factors can cause areas to be warmer or cooler through mechanisms like shading, wind blocking, and heat absorption and reflection.
This document discusses various natural and human factors that can influence climate change. It describes several natural processes such as volcanic eruptions, ocean circulation patterns, solar activity, and Earth's orbital and rotational changes that have short or long-term effects on climate. It also explains how human activities like burning fossil fuels and deforestation have increased greenhouse gases in the atmosphere and led to issues like global warming and ocean acidification. The document provides examples and diagrams to illustrate these concepts and their impacts on climate.
The document summarizes key findings from the IPCC's Fifth Assessment Report regarding climate change projections for South Asia. It finds that human activity is the dominant cause of warming since the 1950s. If emissions continue at a high rate, the Arctic Ocean will likely be ice-free in summers by 2050. South Asia will experience increased temperatures, rainfall, and sea level rise by mid-century, posing challenges for coastal areas, agriculture, and infrastructure. Adaptation and mitigation efforts are needed to reduce impacts.
1) Global warming is caused by increased levels of greenhouse gases like carbon dioxide trapping heat in the lower atmosphere. The thin layer of atmosphere where climate occurs can be influenced by human activity.
2) Human activities like burning fossil fuels have increased atmospheric CO2 levels by about 30% since the industrial revolution, contributing to observed rising global temperatures according to computer models.
3) Potential impacts of unmitigated climate change include rising sea levels, worsening extreme weather, melting ice caps and glaciers, and damage to ecosystems. Reducing emissions from coal power plants, increasing renewable energy and energy efficiency can help address the problem.
The document discusses differences in climate between northern and southern Africa, which are divided by the equator. The northern part includes the Sahara desert, while the southern part includes grasslands. Climate varies in different regions due to geography, with tropical climates near the equator and colder climates farther north and south. Additional factors like altitude, prevailing winds, and distance from the sea also impact regional climates. The document then covers various climate types, weather phenomena, factors influencing climate, and seasonal changes caused by the earth's axial tilt.
The Arctic ecosystem that sustains Arctic residents is melting as temperatures rise, melting permafrost and draining inland freshwater into the ocean. Global warming is increasing temperatures by 3 to 5°C by 2100, rising sea levels by 25 meters, eliminating the Arctic ice cap, and potentially completely melting the Greenland glacier. Increased risks of infectious diseases like malaria, dengue fever, yellow fever, and more frequent cholera outbreaks may also occur due to climate change effects like warmer temperatures.
The document summarizes several effects of climate change that have already been observed and are projected to continue or worsen in the future. Key effects mentioned include rising sea levels and melting polar ice caps destroying animal habitats; longer frost-free seasons and growing seasons affecting ecosystems and agriculture; more frequent and intense heat waves, droughts, and hurricanes; and projections that the Arctic ocean could become ice-free in summer before mid-century while sea levels are expected to rise 1-4 feet by 2100.
Spatio-temporal analyses of the impacts of extreme weather events on renewabl...Global Risk Forum GRFDavos
This document discusses the impacts of extreme weather events on renewable energy infrastructure in Germany. It outlines that heavy rain can damage hydroelectric plants and reduce output. Wind turbines are vulnerable to tornadoes and severe storms. Photovoltaic panels can be disturbed by thunderstorms, hail, high winds and lightning. Germany's climate mitigation concepts aim to integrate risk analyses of extreme weather with analyses of potential renewable energy sites. Regulations for distances between infrastructure and weather risks could be standardized nationwide. The concepts seek to develop sustainable renewable energy systems resilient to climate change impacts.
Climate Change: Implications for CitiesECFoundation
The Fifth Assessment Report from the Intergovernmental Panel on Climate Change is the
most comprehensive and relevant analysis of our changing climate. It provides the scientific fact base that will be used around the world to formulate
climate policies in the coming years.This document is one of a series synthesizing the most pertinent findings of AR5 for specific economic and business sectors. It was born of the belief that the cities sector could make more use of AR5, which is long and highly technical, if it were distilled into an accurate, accessible, timely, relevant and readable summary. Although the information presented here is a ‘translation’ of the key content relevant to this sector from AR5, this summary report adheres to the rigorous scientific basis of the original source material.
Grateful thanks are extended to all reviewers from both the science and business communities for their time, effort and invaluable feedback on this document. The basis for information presented in this overview report can be found in the fully-referenced and peer-reviewed IPCC technical and scientific background reports at: www.ipcc.ch
Sustainable Cities: Urban Impacts of Climate ChangeAnuradha Mukherji
The document discusses the causes and impacts of climate change, as well as strategies for adaptation and mitigation. It notes that increased greenhouse gas emissions since the industrial revolution are changing the composition of the atmosphere and global climate. The impacts of climate change include threats to water resources, energy, infrastructure, food supply, public health, and coastal areas from issues like rising seas and increased extreme weather events. Cities contribute significantly to greenhouse gas emissions but can also play a key role in addressing climate change through resilient planning approaches that incorporate both mitigation and adaptation measures.
Economic Impacts of Extreme Weather Events on Farm Households: Evidence from ...anucrawfordphd
1) The document analyzes the economic impacts of extreme weather events like floods and droughts on farm households in Thailand.
2) It finds that crop income is highly sensitive to rainfall shocks, but households are able to smooth consumption to some degree. Having savings and non-farm income helps households cope with risks.
3) The effects of rainfall shocks vary across households based on their assets and livelihoods. Wealthier households with more diverse income sources are better able to cope with extreme weather impacts.
The document discusses wind power and wind turbines. It explains that wind is created by uneven heating of the earth's surface, and the power of wind is determined by air density, rotor area, and wind speed. There are two main types of wind turbines: horizontal axis wind turbines (HAWT) and vertical axis wind turbines (VAWT). HAWTs are the most common and can have one, two, or three blades mounted on an axis parallel to the ground and to the wind flow. VAWTs have vertical axes and either a Savonius S-shaped design or a Darrieus eggbeater shape. Both turbine types use rotating blades connected to a generator to convert kinetic wind energy into electrical energy.
A master plan or a development plan or a town plan may be
defined as a
general plan for the future layout of a city showing both the existing and
proposed streets or roads, open spaces, public buildings etc. A master
plan is prepared either for improvement of an old city or for a new
town to be developed on a virgin soil. A master plan is a blueprint for the
future. It is an comprehensive document, long-range in its view, that
is intended to guide development in the
township for the next 10 to 20 years.
The document discusses various topics related to town planning and planning concepts including:
- Definitions of town planning and the role of planners
- The planning process including identification of problems, data collection/analysis, forecasting, implementation, and review
- Types of surveys including regional, town, land use, density, and traffic surveys
- Different types of plans including structural, comprehensive, and developmental plans
Adaptations to climate change in the energy sector especially at the renewable energy sector.
Adaptation to climate change in Solar energy
Adaptation to climate change in Wind energy
Adaptation to climate change in Hydro power
Adaptation to climate change in Nuclear energy
It requires less investment when compared to others, Ecofriendly , higher electricity production at cheap cost ,renewable and available all days and nights , Low noise emissions
Advantages of operating in the offshore environment include higher and steadier wind speeds, less-restrictive acoustic requirements, and fewer space constraints.
Infographic: Climate Change and the Energy SectorECFoundation
The Fifth Assessment Report from the
Intergovernmental Panel on Climate Change is the
most comprehensive and relevant analysis of our
changing climate. It provides the scientific fact base
that will be used around the world to formulate
climate policies in the coming years.
This document is one of a series synthesizing the most pertinent findings
of AR5 for specific economic and business sectors. It was born of the belief
that the energy sector could make more use of AR5, which is long and
highly technical, if it were distilled into an accurate, accessible, timely,
relevant and readable summary.
Although the information presented here is a ‘translation’ of the key
content relevant to this sector from AR5, this summary report adheres to
the rigorous scientific basis of the original source material.
The basis for information presented in this overview report can be found in the fully-referenced and peer-reviewed IPCC technical and scientific background reports at: www.ipcc.ch
Climate change - environmental systems and change.Hunter Strike
1) The document discusses evidence of past climate change from various proxy records like tree rings, ice cores, fossils, and historical paintings. It also examines factors that can influence the climate like solar activity, volcanic eruptions, greenhouse gases, and human activities.
2) Climate models project further warming in the coming decades and centuries depending on greenhouse gas emission scenarios, but they have uncertainties regarding changes in extreme events and regional impacts.
3) The climate system is complex and influenced by both natural and human factors interacting across different timescales, making both past and future climate changes difficult to predict precisely.
This document discusses climate change impacts in Wales and the need for adaptation. It summarizes the Met Office's research including operating a high-resolution 1.5km climate model over Wales to better understand local weather extremes and projected changes. The Met Office aims to provide climate services including regional predictions of hazards to help infrastructure planning and resilience in Wales.
Within Interreg project CAMS Platform Ltd. EKODOMA has done research on "Climate Change Adaptation and Mitigation: Practice and Opportunities in Energy Efficiency and Renovation of Buildings in Latvia". Based on the analysis carried out, policy recommendations on planning state support mechanisms and the European structural and investment funds throughout 2021 to 2027, as well as for recommendations on the national guidelines regarding further projects of energy efficiency in renovation and building were developed. The main risks for each of the recommendations have been identified in the authors' view as well.
Climate Change: Implications for EnergyECFoundation
The Fifth Assessment Report from the
Intergovernmental Panel on Climate Change is the
most comprehensive and relevant analysis of our
changing climate. It provides the scientific fact base
that will be used around the world to formulate
climate policies in the coming years.
This document is one of a series synthesizing the most pertinent findings of AR5 for specific economic and business sectors. It was born of the belief
that the energy sector could make more use of AR5, which is long and highly technical, if it were distilled into an accurate, accessible, timely, relevant and readable summary. Although the information presented here is a ‘translation’ of the key content relevant to this sector from AR5, this summary report adheres to the rigorous scientific basis of the original source material.
The basis for information presented in this overview report can be found in the fully-referenced and peer-reviewed IPCC technical and scientific background reports at: www.ipcc.ch
1) The document discusses wind energy utilization globally and the development of offshore wind power in Europe.
2) It provides an overview of the mechanisms that create wind and influence wind patterns near the surface.
3) The document describes different wind turbine technologies as well as substructures used for offshore wind farms.
The document discusses various renewable energy resources including solar power, wind power, hydro power, geothermal energy, and tidal energy. For each energy source, it provides details on how the energy is captured and generated, as well as the pros and cons. It notes that solar remains expensive compared to other renewable sources but that technology advances have increased solar penetration. Wind power has become increasingly competitive but output is unpredictable due to weather. Hydro provides base load power but has environmental and location limitations. Geothermal and tidal energy have large-scale potential but also have specific location and cost constraints.
Wind characteristics, wind speed and energysanthosh kumar
This document discusses various wind characteristics that are important for wind energy production and site selection for wind turbines. It describes:
1) Mean wind speed alone is not sufficient and other factors like wind speed distribution, turbulence, wind direction, and wind shear/profile must be considered.
2) Wind speed patterns can be depicted in a spectrum showing variations over different time periods from minutes to years.
3) The distribution of hourly average wind speeds can be described by a Weibull distribution characterized by a shape and scaling factor.
4) Turbulence or short-term fluctuations in wind speed are important to consider as they can significantly impact energy production and wear on turbines.
For designers to build in resilience and adaptability to meet future climate loads, Building Codes must evolve to include predictive temperature, precipitation, wind, gust, and other environmental loads on buildings. This slide show includes selected information from ECCC on explains the current serious limitations facing designers.
The document discusses how climate change will impact cities through increased temperatures, more extreme precipitation events, and sea level rise. It provides projections for temperature increases and precipitation changes in North America. Cities will experience more heat waves that may be exacerbated by urban heat islands. Coastal cities are particularly at risk from sea level rise. Effective adaptation strategies are needed to reduce risks and increase resilience of cities.
This document discusses small scale wind energy systems. It defines small scale wind turbines as having a swept rotor area less than 200 square meters and being less than 100 kW. It discusses using small wind turbines for off-grid power in remote areas or integrated with buildings. When estimating energy output, it is important to consider the power curve and local wind distribution, which is often weibull. Site conditions like proximity to hills or obstacles can significantly impact wind speed and therefore energy output. Noise and visual impacts are particular concerns for small wind in residential areas.
Small Scale Wind Installations - RETScreen Softwarefernando nuño
This document discusses small scale wind energy systems. It defines small scale wind turbines as having a swept rotor area less than 200 square meters and being less than 100 kW. It discusses using small wind turbines for off-grid power in remote areas or integrated with buildings. When estimating energy output, it is important to consider the power curve and local wind distribution, which is often weibull. Site conditions like proximity to hills or obstacles can significantly impact wind speed and therefore energy output. Noise and visual impacts are particular concerns for small wind in residential areas.
The document summarizes the costs of different energy technologies. It finds that while upfront capital costs are lower for fossil fuels, accounting for additional costs like carbon capture, public health impacts, and climate change effects makes fossil fuels more expensive than renewable sources over the lifetime of the projects. Renewable costs are expected to continue declining due to technological learning and economies of scale, while fossil fuel and nuclear costs are subject to greater uncertainty and overruns. The document concludes that hidden costs are much lower for wind and solar power compared to traditional sources like coal and gas.
The document discusses various renewable energy sources - wind, solar, geothermal, hydroelectric - and their environmental impacts compared to fossil fuels. It finds that while all energy sources have some environmental impact, renewable sources generally cause less harm than fossil fuels in areas like air and water pollution, public health impacts, wildlife effects, and greenhouse gas emissions. Specifically, the life-cycle greenhouse gas emissions are 0.02-0.04 pounds per kWh for wind, 0.07-0.18 pounds per kWh for solar PV, 0.1 pounds per kWh for geothermal, and 0.01-0.5 pounds per kWh for hydro, versus 0.6-3.6 pounds per k
This document describes the fabrication of a revolving gate compressor. It contains a revolving gate that rotates due to human traffic. This rotation is used to turn a compressor through gears, which generates compressed air. The compressed air can then be used for pneumatic applications. It provides a simple and low maintenance method of generating compressed air using human energy from revolving doors.
How climate data can help address the climate challengeEsri UK
Climate change has already altered the weather we experience and the magnitude of impacts from extreme temperatures and rainfall. These impacts manifest locally and can cause human causalities and damage to infrastructure and natural systems. In future, some further climate change is now inevitable, but the rate and magnitude of change will depend on global greenhouse gas emissions. New data and tools to use the data are available to help plot a path through the climate and weather challenges, enabling organisations at all scales to adapt to the changing conditions.
The document discusses field erected cooling towers, which are customized cooling towers designed for large industrial applications. It describes the different types of induced draft cooling towers based on their material of construction, including fiber reinforced polymer (FRP) towers. It emphasizes the importance of considering how the cooling towers will interact with their surrounding environment to prevent issues like recirculation, interference, and poor plume dispersion. Several case studies of large FRP cooling tower installations are presented.
1. IMPACTS OF CLIMATE
AND EXTREME
WEATHER ON ENERGY
INFRASTRUCTURE
Eric Williams
Energy /
Environmental
Economist
International Atomic
Energy Agency
2. OVERVIEW
Climate change (CC) & extreme weather
event (EWE) impacts on energy system
Economic impacts of CC & EWE in the
energy sector
3. CC & EWE
Climate change (CC) = changes in mean and variability
over decades:
Temperature
Precipitation
Wind patterns
Insolation
Sea level rise
Extreme weather events (EWE) = event near the upper or
lower end of the range of observed values (frequency,
intensity, timing) of:
High/low temperature & precipitation
High winds/storms
Hail
Lightning, etc.
4. CC & EWE IMPACTS ON
ENERGY SYSTEM
Extraction/Resource Transport Conversion
Transmission
& Distribution
5. EXTRACTION/RESOURCE
Coal and Uranium:
flooding open-pit mines
dust from coal stockpiles
Oil & gas:
melting permafrost ->
destabilizing equipment
sea level rise: inundating
coastal and offshore sites
See level rise + winds:
damage to onshore wells
and offshore platforms
Hydro:
higher evaporation losses
changes in water availability
Wind:
changes in wind resource
Solar:
changes in insolation
6. TRANSPORT FROM SOURCE
TO CONVERSION
Ocean-going ships:
Less sea-ice = more opportunities for passage
Sea-level rise may affect ports and limit options for large vessels
Inland ships:
Difficult passage for extreme low and extreme high water levels
Rail & roads:
Freeze-thaw cycle leads to damage
High temp: tracks deform; roads soften
Low temp: RR switches freeze; roads crack
Pipelines:
Low temp: can weaken/damage pipelines
High temp: increased corrosion and greater energy requirements for
compression
7. CONVERSION: THERMAL
CC: temps increase
thermal efficiency decreases by 0.1 to 0.2% per 1 C° increase
cooling efficiency decreases: capacity loss of 1 – 2% per 1 C° increase
CC + EWE:
Extreme temp: larger efficiency loss and cooling challenge
Drought: even less and warmer cooling water
Temp & drought: acute cooling problem
Winds: can damage cooling towers
8. CONVERSION: NUCLEAR
CC: same as thermal
Temps go up, thermal and
cooling efficiency goes
down
CC + EWE:
Nuclear is a special case
because of safety concerns
related to EWEs
Although Fukushima was
not climate- or weather-
related, it highlighted the
vulnerability of nuclear
plants to events that were
not considered in design
and construction
9. CONVERSION: NUCLEAR
CC + EWE:
Nuclear plants are built to withstand 50- to
100-year extreme weather events, but as
climate changes, past events may not predict
the severity of future events
Nuclear plants are very complicated systems;
many kinds of EWEs, when combined with an
unknown design or construction flaw, can
trigger safety systems and force a shutdown
Most nuclear plants rely on active safety systems powered
by diesel generators; worst case scenario: an EWE forces a
reactor shutdown while simultaneously, disrupting back up
generators and grid interconnects
10. CONVERSION: NUCLEAR
Lightning: can short-circuit instrumentation,
back-up gen connection, grid connection
High winds: wind-generated missiles can
damage buildings, back-up gen, knock out grid
connection
Extreme cold: ice clogging water cooling intake
Extreme heat: if water for cooling is too hot,
can force shutdown
Flooding: coastal plants vulnerable to storm
surge; inland plants vulnerable to river
flooding; safety systems can be damaged
11. CONVERSION: NUCLEAR
Storm surges and
sea-level rise in
2050:
Key:
Green: no flooding
Yellow: potential flooding
Orange: considerable
flooding
Red: Site inundation
Grey: no data
Source: Kopytko 2007
St.
Lucie
Crystal
River
Turkey
Point
Sea-
Brook
Pil-
grim
Mill-
stone
Calvert
Cliffs
Sea Level Rise
Nor’easter
Category I Low
Category I High
Category II
Category III
Category IV Low
Category IV High
Category V
12. CONVERSION: NUCLEAR
IAEA’s International Reporting
System (IRS)
88% of CC/EWE events affect 3 major
systems
Water cooling: 28%
Electrical control systems: 27%
Transmission grid: 32%
Remainder of events were general (e.g.
flooding)
From 1980 – 1999, events are
balanced between lightning
(33%), winds (33%), and
freezing (30%)
In the 2000s, heat related
events began to appear
15. CONVERSION: HYDRO
CC + EWE:
Flooding: structural damage to dam wall or
turbines from water force and debris
Flooding + winds: waves causing dam
overflow
16. CONVERSION: WIND
CC:
Changes in the spatio-temporal wind resource
distribution; mean wind power densities over
Europe and NA likely within ±50% of current
values
Less frequent icing with increasing temp
Lower precipitation: more dust deposition
Sea level rise: inundating coastal and offshore
sites
17. CONVERSION: WIND
CC + EWE:
Winds: structural damage
Low temps + precipitation: ice formation on blades reducing
efficiency; structural damage
Lightning: structural damage
18. CONVERSION: SOLAR
CC:
Increasing temp: lower PV and CSP
efficiency
Changes in cloudiness and average
insolation
CC + EWE:
Increased precipitation, high winds, hail
and high temperatures can each damage
PV and CSP
Drought + winds: more sand and dust
deposited on collectors, reducing
efficiency of PV and CSP
19. TRANSMISSION &
DISTRIBUTIONRail, road, inland waterways,
pipelines: same issues as
transport from source to
conversion
Electric grid:
CC: decreasing transmission efficiency of 0.4%
per 1 C° increase
CC + EWE:
High temp: lines and transformers overheat, capacity
declines & outages
Low temp: ice -> damage & outages
Lightning: damage & outages
Winds: damage & outages
Flooding: damage & outages
21. COSTS OF NOT ADAPTING
Direct costs:
Physical damage to infrastructure
Reduced output and outages
e.g. every 24 hours a 1 GW unit is shut down costs the owner $1.2
million (assuming $50/MWh)
Indirect costs:
Outages that lead to wider blackouts can impose
substantial indirect costs
Value of lost load in developed countries ranges from 200 to 960
million euros for a 24 hour blackout (based on lost output for a 1
GW plant) (Nooij et al. 2007, Tol 2007)
Cumulative macroeconomic costs from physical
damage, need for additional capacity, outages, etc.
22. ADAPTATION OPTIONS
Investments in adaptation can avoid or
mitigate some costs
Options too numerous to catalogue here
General approaches fall within 3 categories
Physical protection
e.g. building sea walls and other earthworks to protect
coastal energy infrastructure from sea-level rise and
storm surges
Alternative technologies
e.g. dry cooling for thermal power plants
Alternative operational strategies
e.g. sophisticated computer modeling to better manage
hydropower resources under changing rainfall patterns
23. CC: DECENT COVERAGE IN
STUDIES
○ = not modelled
● = modelled Wind Solar Hydro Thermal Nuclear Grid Coal
Oil &
Gas
Higher mean
temperatures* ○ ○ ○ ● ● ● ○
Changes in rainfall
patterns ● ● ●
Changes in wind
patterns ●
Changes in average
insolation ●
24. CGE STUDIES: PRIMARILY
GRADUAL CLIMATE CHANGE
GDP impacts in most studies on the
order of -1% in 2050+ but up to -3%
With some assumptions about
adaptation investments, studies find that
GDP impacts can be close to zero
Not based on specific adaptation measures, so
these results are questionable
Warmer regions tend to have a greater
impact than cooler regions
25. PARTIAL EQUILIBRIUM
STUDIES: CC
Results not in terms of GDP, but mostly
consistent with CGE results when
examining longer-term gradual climate
change
~1% increase in electricity demand in warmer countries
~1% decrease in demand in cooler countries
26. MODELING EXTREME
WEATHER EVENTS
Extreme weather events occur with a low
probability (perhaps increasing with CC) and
are difficult to model
One approach is to make a general assumption
about aggregate impacts of extreme weather
Done in one study (Jochem and Schade et al. 2009)
Another approach is to develop probabilities of
events with varying intensity and
corresponding damages and include them
stochastically within a detailed technology-
based energy model
To date, this approach has not been taken
28. PARTIAL EQUILIBRIUM
MODELS: EWE
More significant impacts with extreme
weather
Electricity prices in Nordic countries can
double over a 2 year period during a
hypothetical water shortage scenario (Bye et
al. 2006)
A drought scenario in the US southwest can
lead to average monthly electricity prices that
are 8% (November) to 24% (July) higher
(DOE/NETL 2009)
Boyd and Ibarraran 2009 evaluate drought
scenarios in Mexico and find that in 2026
generation output declines -2.1% but with
29. LIMITED STUDIES FOR
DEVELOPING COUNTRIES
Only a couple of studies of the impacts of
climate change and extreme weather in
developing countries
Lucena et al. 2010 model reduced hydropower from
altered rainfall and rising temps that affect thermal
efficiency and energy demand
CCEWE lead to needing an addition 153 to 162 TWh of
electricity per year
Capital investment needed to cover generation amounts to
$48 to $51 billion … equivalent to 10 years of capital
expenditures in Brazil’s long-term energy plan
An additional ~$7 billion per year also needed for operating
expenses
Boyd and Ibarraran 2009 evaluate drought
scenarios in Mexico and find that in 2026
generation output declines -2.1% but with
adaptation can increase by 0.24%
30. OVERALL CONCLUSIONS
CC: mostly affects the resource base of
renewables
CC: the impacts on thermal and rest of supply
chain are not severe
CC + EWE: the impacts can be severe
throughout energy supply chain
Although nuclear is generally resilient, the safety concerns
posed by EWEs must be taken seriously
The costs of CC + EWE have not been
adequately evaluated, particularly EWEs
The limited studies on EWEs suggest that impacts can be
significant
Few studies have been done on the CC + EWE impacts on the
31. LOOKING AHEAD
IAEA has begun a coordinated research project with
institutions in:
Argentina
Cuba
Egypt
China
Ghana
Pakistan
Slovenia
Sudan
Goal of the research is to identify vulnerabilities of
energy infrastructure in each country as well as cost-
effective adaptation options
37. Study
Model
Type Climate Impacts Modeled Energy/Economic Impacts
Regi
ons
Sect
ors
Stud
ied
Bosello et
al. 2009 IAM
Rising temperatures/ changing demand for
energy; impacts from 4 other sectors/events
(Global, 2001 - 2050)
Change in GDP in 2050 due to rising temperatures and
changing energy demand: 0% to 0.75% (+1.2°C); -0.1% to
1.2% (+3.1°C) 14 4
Jorgenso
n et al.
2004 CGE
Rising temperatures/ changing demand for
energy; climate impacts from 3 other sectors
(USA, 2000 - 2100)
Optimistic adaptation: 4% to 6.7% higher energy
productivity per year (2000 – 2100); Output from
electricity: -6% in 2050; GDP is +0.7% (aggregate all
sectors, avg annual 2000 – 2100)
Pessimistic adaptation: 0.5% to 2.2% lower energy
productivity per year; Output from electricity: +2% in 2050;
GDP is -0.6% (aggregate impact all sectors) 1 35
Bosello et
al. 2007 CGE
Rising temperatures/ changing demand for
energy (Global, 2050)
Change in GDP in 2050 (perfect competition): -0.297% to
0.027%;
Change in GDP in 2050 (imperfect competition): -0.303% to
0.027% 8 1
Aaheim
et al.
2009 CGE
Change in precipitation -> share of hydro power;
rising temperatures/ changing demand for
energy ; impacts from 4 other sectors (Western
Europe, 2071 – 2100)
Impact from all sectors in 2100: GDP in cooler regions: -1%
to -0.25%
GDP in warmer regions: -3% to -0.5%
Adaptation can mitigate 80% to 85% of economic impact 8 11
Generation output in 2026: -2.1%
Refining output: -10.1%
Coal output: -7.8%
NG output: -2%
Crude oil output: +1.7%
GDP: -3%
With adaptation:
Generation output in 2026: 0.24%%
Refining output: 1.36%%
Coal output: 1.09%%