The United States is engaged in extensive international efforts on climate change. EPA actively participates in multilateral and bilateral activities by establishing partnerships and providing leadership, technical expertise and capacity building support. Multilaterally, the United States is the largest funder of activities under the United Nations Framework Convention on Climate Change (UNFCCC) and the Intergovernmental Panel on Climate Change (IPCC). The U.S. remains fully committed to multilateral action under the UNFCCC, and has created or worked to revitalize a range of international climate initiatives within the last two years.

• Multilateral Activities (more than two countries)
• Bilateral Activities (between two countries)
• UNFCCC Commitments

As a Party to the UNFCCC, the United States shares with other countries its ultimate objective: stabilization of greenhouse gas concentrations in the atmosphere at a level that prevents dangerous human-induced interference with the climate system. In February 2002, President Bush reaffirmed America’s commitment to the Framework Convention and its central goal, while also making clear that he could not commit the U.S. to the Kyoto Protocol. The United States decided not to ratify the Kyoto Protocol because it does not mandate emissions reductions from all countries (some of which are major trading partners) and as a result, could damage the economy. Recent analysis from the U.S. Climate Change Science Program suggests that greenhouse gas emissions from developing countries are expected to exceed emissions from developed countries within the next 25 years. More information on the Kyoto Protocol.

EPA - INTERNATIONAL IMPACT SUMMARY

(MUST CONFIRM WITH DATA)

Many global issues are climate-related and thus may be affected by climate change. These include water resource availability and food security, especially for areas already afflicted by drought and extreme weather events. Sea-level rise is a particular concern for low-lying coasts and island nations.

Some nations will likely experience more adverse effects than others, while other nations may benefit. Poorer nations are generally more vulnerable to the consequences of global warming. These nations tend to be more dependent on climate-sensitive sectors, such as subsistence agriculture, and may lack the resources to buffer themselves against the changes that global warming may bring.

The Intergovernmental Panel on Climate Change (IPCC) has examined a range of future climate change scenarios and found that the globally averaged surface air temperature is projected by models to warm 2 to 11.5°F (1.1-6.4°C) by 2100 relative to 1990, and globally averaged sea level is projected by models to rise 7.2 to 23.6 inches (18-59 cm or 0.18- 0.59m) by 2100. The warming would vary by region, and would be accompanied by changes in precipitation, changes in the variability of climate, and changes in the frequency and intensity of some extreme climate phenomena. (IPCC, 2007)

TOHOKU ELECTRIC POWER - Participation in Japan GHG Reduction Fund

(FACT - Actual fund started in Japan)

TOHOKU ELECTRIC POWER - Purchase of CO2 Credits from Biomass Power Generation Project (Honduras)

(FACT - Actual project started in Honduras)

TOHOKU ELECTRIC POWER - Participation in Afforestation Project Overseas (Australia)

(FACT - Actual project started in Australia)

TOHOKU ELECTRIC POWER - Co-Generation and Energy-Saving Model Project (Kazakhstan)

(FACT - Actual project started in Kazakhstan)

EPA - INTERNATIONAL IMPACT

(MUST CONFIRM WITH DATA)

The IPCC has identified specific impacts for the following regions:

Several countries have also done national assessments of climate change impacts - see the related links box for examples of these national assessments.

Highlights of Projected Regional Impacts

The projected impacts shown below are drawn from the IPCC’s Summary for Policymakers, Working Group II and reflect information in the regional chapters listed above.

Africa

• New studies confirm that Africa is one of the most vulnerable continents to climate variability and change because of multiple stresses and low adaptive capacity.
• By 2020, between 75 million and 250 million people are projected to be exposed to increased water stress due to climate change.
• Agricultural production, including access to food, in many African countries and regions is projected to be severely compromised by climate variability and change.
• Toward the end of the 21st century, projected sea-level rise will affect low-lying coastal areas with large populations.

Asia

• Glacier melt in the Himalayas is projected to increase flooding, increase rock avalanches from destabilized slopes, and affect water resources within the next two to three decades.
• Freshwater availability in Central, South, East and Southeast Asia, particularly in large river basins, is projected to decrease due to climate change, which, along with population growth and increasing demand from higher standards of living, could adversely affect more than a billion people by the 2050s.
• Coastal areas, especially heavily populated megadelta regions in South, East and Southeast Asia, will be at greatest risk due to increased flooding from the sea and, in some megadeltas, flooding from rivers.
• Crop yields could increase up to 20 percent in East and Southeast Asia, while they could decrease up to 30 percent in Central and South Asia by the mid-21st century.
• Sickness and death due to diarrheal disease, primarily associated with floods and droughts, are expected to rise in East, South and Southeast Asia due to projected changes in the hydrological cycle associated with global warming.

Australia and New Zealand

• Water security problems are projected to intensify by 2030 in parts of Australia and New Zealand.
• Significant loss of biodiversity is projected to occur by 2020 in some ecologically rich sites, including the Great Barrier Reef and Queensland Wet Tropics.
• Coastal development and population growth, in areas such as Cairns and Southeast Queensland (Australia) and Northland to Bay of Plenty (New Zealand), are projected to exacerbate risks from sea-level rise and increases in the severity and frequency of storms and coastal flooding by 2050.
• Production from agriculture and forestry by 2030 is projected to decline over much of southern and eastern Australia, and over parts of eastern New Zealand, due to increased drought and fire. However, in New Zealand, initial benefits are projected in western and southern areas and close to major rivers due to a longer growing season, less frost and increased rainfall.

Europe

• For the first time, wide-ranging impacts of changes in current climate have been documented in Europe: retreating glaciers, longer growing seasons, shift of species ranges, and health impacts due to a heatwave of unprecedented magnitude.
• Nearly all European regions are anticipated to be negatively affected by some future impacts of climate change, and these will pose challenges to many economic sectors.
• In Southern Europe, climate change is projected to worsen conditions (high temperatures and drought) in a region already vulnerable to climate variability, and to reduce water availability, hydropower potential, summer tourism and, in general, crop productivity.
• In Central and Eastern Europe, summer precipitation is projected to decrease, causing higher water stress. Health risks due to heatwaves are projected to increase. Forest productivity is expected to decline and the frequency of peatland fires to increase.
• In Northern Europe, climate change is initially projected to bring mixed effects, including some benefits such as reduced demand for heating, increased crop yields, and increased forest growth. However, as climate change continues, its negative impacts (including more frequent winter floods, endangered ecosystems and increasing ground instability) are likely to outweigh its benefits.

Latin America

• By mid-century, increases in temperature and associated decreases in soil water are projected to lead to gradual replacement of tropical forest by savanna in eastern Amazonia.
• In drier areas, climate change is expected to lead to salinization and desertification of agricultural land. Productivity of some important crops is projected to decrease and livestock productivity to decline, with adverse consequences for food security. In temperate zones, soybean yields are projected to increase.
• Sea-level rise is projected to cause increased risk of flooding in low-lying areas.
• Changes in precipitation patterns and the disappearance of glaciers are projected to significantly affect water availability for human consumption, agriculture, and energy generation.

North America

• Warming in western mountains is projected to cause decreased snowpack, more winter flooding, and reduced summer flows, exacerbating competition for over-allocated water resources.
• Disturbances from pests, diseases, and fire are projected to have increasing impacts on forests, with an extended period of high fire risk and large increases in area burned.
• Moderate climate change in the early decades of the century is projected to increase aggregate yields of rain-fed agriculture by 5- 20 percent, but with important variability among regions. Major challenges are projected for crops that are near the warm end of their suitable range or which depend on highly utilized water resources.
• Cities that currently experience heatwaves are expected to be further challenged by an increased number, intensity and duration of heatwaves during the course of the century, with potential for adverse health impacts. Elderly populations are most at risk.
• Coastal communities and habitats will be increasingly stressed by climate change impacts interacting with development and pollution.

Polar Regions

• The main projected biophysical effects are reductions in thickness and extent of glaciers and ice sheets, and changes in natural ecosystems with detrimental effects on many organisms including migratory birds, mammals and higher predators. In the Arctic, additional impacts include reductions in the extent of sea ice and permafrost, increased coastal erosion, and an increase in the depth of permafrost seasonal thawing.
• For human communities in the Arctic, impacts, particularly those resulting from changing snow and ice conditions, are projected to be mixed. Detrimental impacts would include those on infrastructure and traditional indigenous ways of life. Beneficial impacts would include reduced heating costs and more navigable northern sea routes.
• In both polar regions, specific ecosystems and habitats are projected to be vulnerable, as climatic barriers to species invasions are lowered.

Small Islands

• Small islands, whether located in the tropics or higher latitudes, have characteristics that make them especially vulnerable to the effects of climate change, sea-level rise, and extreme events.
• Deterioration in coastal conditions, for example through erosion of beaches and coral bleaching, is expected to affect local resources, e.g., fisheries, and reduce the value of these destinations for tourism.
• Sea-level rise is expected to exacerbate inundation, storm surge, erosion, and other coastal hazards, thus threatening vital infrastructure, settlements, and facilities that support the livelihood of island communities.
• Climate change is projected by mid-century to reduce water resources in many small islands, e.g., in the Caribbean and Pacific, to the point where they become insufficient to meet demand during low-rainfall periods.
• With higher temperatures, increased invasion by non-native species is expected to occur, particularly on mid- and high-latitude islands.