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Solar cycles and changes in the sun s radiation affect local climate and allow the sun s energy to reach the Earth s surface, keeping heat from escaping The Earth gets slowly hotter Industrial activity produces greenhouse gases, which serve as additional blankets to heat the Earth even more The enhanced greenhouse effect caused by the burning of fossil fuels (oil, coal, and natural gas) increases global warming and changes the environment
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Global warming effects differ around the world and make it hard to predict exactly how the climate may change Temperature increases are expected to be higher in polar areas than around the equator Land temperatures might be higher than those over oceans Rainfall might be heavier in some areas and lower in others Major climatic change greatly affects local weather through the frequency and intensity of storms Some scientists fear the high number of major Atlantic hurricanes in recent years may be the beginning of severe climate change Ranching, crops, pests, diseases, ocean levels, and native plant and animal populations would all be impacted Increasing global warming has also motivated people in different cities, states, industries, and countries to step up their work on developing clean energy options
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Carbon is essential to life, but increasingly a problem as fossil fuel burning increases atmospheric carbon dioxide However, unless you live in a polluted city or near industrial plants, it s hard to believe the Earth s immense atmospheric layers can t handle industrial pollutants Global warming is often dismissed as a knee-jerk reaction of environmentalists In 2004, scientists reported in Science that the ocean had taken up nearly half of the carbon dioxide gas released into the air since the 1800s This was good news, since less greenhouse gases means less global warming However, oceans will reach their carbon dioxide limit Carbon uptake starts with plankton These tiny organisms, drifting along on ocean currents, perform photosynthesis to produce energy and draw carbon out of the atmosphere While building intricate calcium carbonate shells, they bind carbon as well Eventually, these organisms die and sink to the bottom of the ocean dropping out of the carbon cycle The rest dissolve in the low-calcium carbonate conditions of deep waters Either way, their carbon doesn t return to the atmosphere for a very long time Carbon sequestration removes and stores atmospheric carbon in carbon sinks (eg, oceans, forests) through physical and biological processes like photosynthesis
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The amount of human-produced carbon dioxide being absorbed into the ocean is important If carbon dioxide levels get high enough, the ocean s top layer will become more acidic, reducing calcium carbonate s availability to plankton Then, as human-produced carbon dioxide sinks into the ocean, calcium carbonate dissolution may speed up This becomes especially significant when shell-making is impacted In the last decade, scientists found that even small calcium carbonate decreases in seawater limited plankton s and coral s ability to build exoskeletons If this continues over more centuries, organisms ability to create shells may be compromised If sinking shells from dead organisms dissolve in this shallower ocean water and their carbon returns into the atmosphere a lot sooner, the greenhouse effect will accelerate dramatically The take home message is: if oceans become less effective as a sink for human-produced carbon dioxide, the buildup of atmospheric carbon dioxide will accelerate
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We ve seen how the combustion of coal, oil, and natural gas cause global CO2 levels to rise Less well known is how trees absorb CO2 during photosynthesis and then release it when they are cut down The 34 million acres of tropical forests destroyed annually, about the size of New York state, release between 20% to 25% of total global CO2 emissions In 1992, at the United Nations Earth Summit in Rio de Janeiro, the international community first acknowledged the threat of climate instability Over 185 nations agreed to reduce greenhouse gas emissions to their 1990 levels by 2012 More importantly, the participants agreed to stabilize atmospheric concentrations of greenhouse gases to prevent dangerous human interference with the global climate system The US Environmental Protection Agency s Clean Air Markets Division developed the annual Inventory of US Greenhouse Gas Emissions and Sinks This EPA atmospheric inventory estimates, documents, and evaluates greenhouse gas emissions and sinks for all source categories To update the report, the Inventory Program polls dozens of federal agencies, academic institutions, industry associations, consultants, and environmental organizations for up-to-date information It also gets data from a network of continuous carbon dioxide emission monitors installed at most US electric power plants In December 2008, the Department of Energy reported total US greenhouse gas emissions of CO2 levels rose by 17% from 1990 to 2007 If business-as-usual industrial output doesn t change, global CO2 levels will double by the end of the 21st century Under the umbrella of the Intergovernmental Panel on Climate Change (IPCC), over 200 scientists and national experts worked together to develop guidelines to help countries create atmospheric inventories across international borders Since then, scientists determined that stabilizing atmospheric levels of carbon dioxide will mean reducing CO2 emissions and other heat-trapping gases to 80% of the 1990 global levels According to some models, this means decreasing or stopping the release of 12 trillion tons of CO2 by 2050 This isn t an impossible mission Better energy efficiency throughout the global economy could prevent one-third of emissions while cutting energy costs Scientists use natural and industrial emission inventories as tools to develop atmospheric models Policy makers and regulatory agencies use these inventories to check policy compliance and emission rates Most inventories contain the following information: Chemical and physical identity and properties of pollutants Geographical area affected Time period when emissions were generated
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