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Global Climate Change Digest A Guide to Information on Greenhouse Gases and Ozone Depletion Published July 1988 through June 1999
Atlanta's Changing Storm Climate (JUNE 1999)
Item #d99jun45
In the summer, the Southeast regularly experiences afternoon
thunderstorms. Atlanta, however, has also had predawn or early morning
showers that continue until noon. At the annual meeting of the Association
of American Geographers in Honolulu, Hawaii, on Mar. 24, 1999, Robert
Bornstein and Qing Lu Lin from San Jose State University in California
attributed this anomalous pattern to urban heat islands that heat the air
5 to 8 degrees (Fahrenheit) higher than in outlying areas, causing it to
rise. The cooler, outlying air is then sucked in to replace the rising air
mass. As the warm air ascends, the water in it cools and condenses,
producing intense and localized rainstorms with thunder and lightning. The
early morning rain results because the urban heat islands retain their
high temperature long after nightfall. Indeed, aircraft data indicate that
the pavement of parking lots can reach 120°F during the day; tree-shaded
areas in the same locale only reach 89°F. Planting trees and installing
highly reflective roofing materials are recommended ways to ameliorate the
effects of such heat islands.
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