Link between El Ninos and droughts in India.Scientists report that droughts in India are associated with a particular type of El Nino, the climate phenomenon marked by increased sea-surface temperatures in the tropical Pacific. The rainy rain·y adj. rain·i·er, rain·i·est Characterized by, full of, or bringing rain. rain  i·ness n.Adj. season in India occurs in June, July, and August. Between 1871 and 2002, central India experienced 10 severe summertime droughts, says Martin Hoerling, a meteorologist with the National Oceanic and Atmospheric Administration Noun 1. National Oceanic and Atmospheric Administration - an agency in the Department of Commerce that maps the oceans and conserves their living resources; predicts changes to the earth's environment; provides weather reports and forecasts floods and hurricanes and in Boulder, Colo. Every one of those dry spells occurred during an El Nino, he notes. However, not all El Ninos during that 132-year period caused droughts--in 13 cases, summer rainfall during an El Nino was at or slightly above normal. The explanation, says Hoerling, is that not all El Ninos are the same. While some primarily warm up the eastern Pacific near South America South America, fourth largest continent (1991 est. pop. 299,150,000), c.6,880,000 sq mi (17,819,000 sq km), the southern of the two continents of the Western Hemisphere. , the hot spots hot spots acute moist dermatitis. for other El Ninos appear mainly in the central Pacific. Indian droughts seem to result from only the latter type, Hoerling and his colleagues report online and in an upcoming Science. Warmer-than-normal ocean temperatures in the central Pacific send large amounts of moist, warm air up to high altitudes Conventionally, an altitude above 10,000 meters (33,000 feet). See also altitude. there. This shift in the atmosphere causes air masses to move downward over central India, climate models suggest. Such downwelling Downwelling is the process of accumulation and sinking of higher density material beneath lower density material, such as cold or saline water beneath warmer or fresher water or cold air beneath warm air. It is the sinking limb of a convection cell. tends to suppress rainfall. Few studies have scrutinized central-Pacific El Ninos, says Hoerling. A better understanding of that type may enable scientists to develop an early-warning system for Indian droughts, he notes. |
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