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The Urban Heat Island and Local Temperature Variations in Orlando, Florida

The Urban Heat Island and Local Temperature Variations in Orlando, Florida Cities artificially alter local climates affecting economic and biological processes. This study examined air temperatures in Orlando's urban canopy layer using a network of twenty-nine fixed-point stations from September 1999 to December 2001. Urban Heat Island (UHI) statistics were calculated using two stations that were representative of an urban and rural setting. Orlando's UHI develops best on calm, clear nights during dry months: its maximum magnitude exceeds 8°C. Orlando's UHI, however, is predominantly a nocturnal phenomenon with intense heat islands sometimes occurring during warm afternoons. These events are most likely attributable to isolated thundershowers. Local temperature variations between urban and rural extremes were examined by calculating environmental indices for all stations. The range in monthly cooling degreeday totals exceeded 100 degree days in six months of the thirty-six month study period. Heating degree totals and number of freezing hours were also highly variable. http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Southeastern Geographer University of North Carolina Press

The Urban Heat Island and Local Temperature Variations in Orlando, Florida

Southeastern Geographer , Volume 46 (2) – May 10, 2006

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Publisher
University of North Carolina Press
Copyright
Copyright © 2006 by the Southeastern Division, Association of American Geographers.
ISSN
1549-6929
Publisher site
See Article on Publisher Site

Abstract

Cities artificially alter local climates affecting economic and biological processes. This study examined air temperatures in Orlando's urban canopy layer using a network of twenty-nine fixed-point stations from September 1999 to December 2001. Urban Heat Island (UHI) statistics were calculated using two stations that were representative of an urban and rural setting. Orlando's UHI develops best on calm, clear nights during dry months: its maximum magnitude exceeds 8°C. Orlando's UHI, however, is predominantly a nocturnal phenomenon with intense heat islands sometimes occurring during warm afternoons. These events are most likely attributable to isolated thundershowers. Local temperature variations between urban and rural extremes were examined by calculating environmental indices for all stations. The range in monthly cooling degreeday totals exceeded 100 degree days in six months of the thirty-six month study period. Heating degree totals and number of freezing hours were also highly variable.

Journal

Southeastern GeographerUniversity of North Carolina Press

Published: May 10, 2006

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