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global warming |
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global warming![]() The warming effect of the Earth's atmosphere is called the greenhouse effect. Radiation from the Sun enters the atmosphere but is prevented from escaping back into space by gases such as carbon dioxide (produced for example, by the burning of fossil fuels), nitrogen oxides (from car exhausts), and CFCs (from aerosols and refrigerators). As these gases build up in the atmosphere, the Earth's average temperature is expected to rise. Increase in average global temperature of approximately 0.5°C/0.9°F over the past century. Much of this is thought to be related to human activity. Global temperature has been highly variable in Earth history and many fluctuations in global temperature have occurred in historical times, but this most recent episode of warming coincides with the spread of industrialization, prompting the suggestion that it is the result of an accelerated greenhouse effect caused by atmospheric pollutants, especially carbon dioxide gas. The melting and collapse of the Larsen Ice Shelf, Antarctica, since 1995, is a consequence of global warming. Melting of ice is expected to raise the sea level in the coming decades. Natural, perhaps chaotic, climatic variations have not been ruled out as the cause of the current global rise in temperature, and scientists are still assessing the influence of anthropogenic (human-made) pollutants. In 1988, the World Meteorological Organization (WMO) and the United Nations (UN) set up the Intergovernmental Panel on Climate Change (IPCC), a body of more than two thousand scientists, to investigate the causes of and issue predictions regarding climate change. In June 1996, the IPCC confirmed that global warming was taking place and that human activities were probably to blame. Assessing the impact of humankind on the global climate is complicated by the natural variability on both geological and human time scales. The present episode of global warming has thus far still left England approximately 1°C/1.8°F cooler than during the peak of the so-called Medieval Warm Period from 1000 to 1400. The latter was part of a purely natural climatic fluctuation on a global scale. The interval between this period and the recent rise in temperatures was unusually cold throughout the world, relative to historical temperatures. Scientists predict that a doubling of carbon dioxide concentrations, expected before the end of the 21st century, will increase the average global temperature by 1.4-5.8°C/2.5-10.4°F. In addition to a rise in average global temperature, global warming has caused seasonal variations to be more pronounced in recent decades. Examples are the most severe winter on record in the eastern USA 1976-77, and the record heat waves in the Netherlands and Denmark the following year. Mountain glaciers have shrunk, late summer Arctic sea-ice has thinned by 40%, and sea levels have risen by 10-20 cm/4-8 in. Scientists have predicted a greater number of extreme weather events, and sea levels are expected to rise by 9-88 cm/4-35 in by 2100. 1998 was the warmest year globally of the last millennium, according to US researchers who used tree rings and ice cores to determine temperatures over the past 1,000 years.
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