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Global Warming
Variations in the energy output of the sun, changes in the relative positions of the sun and Earth, shifting locations of the continents, volcanic eruptions, and other alterations of atmospheric composition all combine to cause climate change. The long term changes in Earth's temperatures are encompassed within a range of natural variability. However, global warming refers to the relatively rapid, recent changes that are outside this range of natural variability. The mean global temperature of Earth has not deviated more than 1 degree Celsius from the average since the beginning of civilization. By 2100, Earth's temperature is forecast to increase from 1.5 to 4 degrees Celsius if present rates of warming continue. This rate of temperature increase is unequivocal in that it has no equal in the past half million years. The evidence for global warming is overwhelming, and includes melting glaciers and sea ice, rising sea level, increased heights of storm surges, a greater frequency of severe weather events (including category 4 and 5 hurricanes), an increased number and severity of floods, droughts, and wild fires, and an increase in the acidity of the world's oceans.
The burning of fossil fuels and deforestation during the last 100 years has increased the level of carbon dioxide (CO2) from 280 parts per million (ppm) to 390 ppm, and CO2 is a potent greenhouse gas. Countries around the globe have convened to find a resolution to this pressing problem as they met in Kyoto, Japan, in 1997, Copenhagen, Denmark, in 2009, and in Cancun, Mexico, in 2010. The Intergovernmental Panel on Climate Change (IPCC) is a body of more than 2,000 of the world's foremost atmospheric scientists, and is held to be a reliable source of information on all aspects of global warming. In their fourth assessment report published in 2007, these experts outlined the importance of the choices made by societies in determining the degree to which the planet will continue to warm in their “Special Report on Emission Scenarios” (SRES). The atmosphere will continue to warm throughout the next century. However, the boldness and efficiency with which individuals and governments act will make a substantial difference in the depth of the disasters that will ensue.
The Causes
The global population has grown to such an extent in absolute numbers and in per capita footprint that extensive surface changes have been created by human activity. For example, the intense development found in cities is so pronounced that a new set of climatic conditions is created, called the urban heat island effect. Because global wind patterns and ocean currents effectively redistribute heat energy, the climate of the entire planet is being altered. In fact, higher latitudes are experiencing far greater warming than are lower latitudes. Such extensive change has the potential to move our planet to a new stage unknown in human history, and to entirely revise socioeconomic systems.
In the developed world, economies are largely driven by fossil fuels. The developing world is increasingly relying on fossil fuels as well. The preponderance of electricity is generated through coal-fired power plants. Crude oil is used to provide space heat in homes and office buildings, and is refined to make gasoline to power automobiles and trucks. Fossil fuels were formed over the course of millions of years, when organic matter became covered with sediments and became buried in fossil rock. When those fuels are drilled, mined, and burned, the carbon that was stored for eons is released back into the atmosphere very rapidly. Presently, the burning of organic compounds is adding far greater amounts of CaO2 to the atmosphere than photosynthesis on land or in the oceans can remove. Approximately 8 billion tons of CO2 are added to the atmosphere each year, and about half is removed by the oceans and vegetation on land. Consequently, approximately 4 billion tons of CO2 are added to the atmosphere annually. By the year 2025, the amount of CO2 added annually is expected to increase to between 9 and 15 billion tons. For years beyond 2025, estimates are highly variable, due to uncertainties about whether the countries with major emissions will take steps to reduce their output of greenhouse gases. If not, emission levels by 2100 could be five times as high as today.
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- Africa, North
- Africa, Sub-Saharan
- Asia, East
- Asia, West, Central, and South
- Australia and Pacific Region
- Canada
- Caribbean Island Region
- China
- Desertification
- Earthquake Zones
- Europe, Eastern
- Europe, Western
- Evacuation Routes
- Glacial Melt
- Hurricane Zones
- Japan
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- Mexico
- Middle East
- Ring of Fire
- Russia
- South America
- United Kingdom
- United States, California and West Coast
- United States, Great Lakes
- United States, Hawaii and Pacific Territories
- United States, Mid-Atlantic
- United States, Midwest
- United States, Mountain States
- United States, National
- United States, Northeast
- United States, Northwest and Northern Plains
- United States, Southeast and Gulf Coast
- United States, Southwest
- American Red Cross
- Center for International Disaster Information (CIDI)
- Centers for Disease Control and Prevention (CDC)
- ChildFund International
- Coast Guard, U.S.
- Cooperative for Assistance and Relief Everywhere (CARE)
- Defense, U.S. Department of Direct Relief
- Disaster Preparedness and Emergency Response Associations
- Doctors Without Borders
- Federal Emergency Management Agency (FEMA)
- Food and Agriculture Organization of the United Nations (FAO)
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- InterAction
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- International Medical Corps
- International Red Cross
- Interpol
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- National Governments
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- World Concern
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- World Food Program
- World Health Organization (WHO)
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- History of Disaster Relief, Africa
- History of Disaster Relief, Ancient World
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- History of Disaster Relief, Europe
- History of Disaster Relief, India
- History of Disaster Relief, Middle East
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- Exercise Planning
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- Mass Casualty Management
- Media
- National Incident Management System (NIMS)
- National Standards
- Packaging and Tracing of Food
- Paramedics
- Political Economy of Food
- Provision of Food in Disasters
- Refugee Policy
- Refugees, Care of
- Reserve Storage and Transport
- Transportation
- Vulnerable Populations
- Incentives, Intergovernmental and Intersystem
- Mitigation, Benefits and Costs of
- Private Sector, Role in Mitigation
- Public Sector, Role in Mitigation
- Public-Private Interactions in Mitigation
- Regulatory Approaches to Mitigation
- Risk, Government Assumption of
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- Structural (Engineering) Options for Mitigation
- Avalanches
- Diseases
- Droughts
- Earthquakes
- Fires, Forest
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- Floods
- Heat Waves
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- Landslides
- Pest Invasions
- Sea Surges
- Tornadoes
- Tsunamis
- Volcanoes
- Winter Storms
- Bilateral Versus Multilateral Aid
- Domestic Corruption in International Disasters
- Domestic Politics in International Disasters
- Donations, National
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- Funding of International Relief
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- Politics in International Funding
- Rejection of International Aid
- Intergovernmental Relations and Preparedness
- Planning for Disasters, International
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- Planning for Disasters, National
- Political Support for Preparedness
- Preparedness, Function of
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- Research-Based Disaster Planning
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- Recovery, Phases of
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- Response, Management Strategies
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- Data Processing
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- Funding, U.S.
- Global Warming
- Modeling
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- Real-Time Communications
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- Cross-Cultural Interactions
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- Disaster Experience
- Education
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- Gender and Disasters
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- Risk Communications
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- United States, California and West Coast
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- United States, Hawaii and Pacific Territories
- United States, Mid-Atlantic
- United States, Midwest
- United States, Mountain States
- United States, National
- United States, Northeast
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