The Impact of the Urban Heat Island during an Intense Heat Wave in Oklahoma City

During late July and early August 2008, an intense heat wave occurred in Oklahoma City. To quantify the impact of the urban heat island (UHI) in Oklahoma City on observed and apparent temperature conditions during the heat wave event, this study used observations from 46 locations in and around Okla...

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Main Authors: Jeffrey B. Basara, Heather G. Basara, Bradley G. Illston, Kenneth C. Crawford
Format: Article
Language:English
Published: Hindawi Limited 2010-01-01
Series:Advances in Meteorology
Online Access:http://dx.doi.org/10.1155/2010/230365
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spelling doaj-330ae57eb2c640e7a34ebc57aff6ae302020-11-25T00:39:13ZengHindawi LimitedAdvances in Meteorology1687-93091687-93172010-01-01201010.1155/2010/230365230365The Impact of the Urban Heat Island during an Intense Heat Wave in Oklahoma CityJeffrey B. Basara0Heather G. Basara1Bradley G. Illston2Kenneth C. Crawford3Oklahoma Climatological Survey, University of Oklahoma, Norman, OK 73072, USACenter for Applied Social Research, University of Oklahoma, Norman, OK 73072, USAOklahoma Climatological Survey, University of Oklahoma, Norman, OK 73072, USAOklahoma Climatological Survey, University of Oklahoma, Norman, OK 73072, USADuring late July and early August 2008, an intense heat wave occurred in Oklahoma City. To quantify the impact of the urban heat island (UHI) in Oklahoma City on observed and apparent temperature conditions during the heat wave event, this study used observations from 46 locations in and around Oklahoma City. The methodology utilized composite values of atmospheric conditions for three primary categories defined by population and general land use: rural, suburban, and urban. The results of the analyses demonstrated that a consistent UHI existed during the study period whereby the composite temperature values within the urban core were approximately 0.5∘C warmer during the day than the rural areas and over 2∘C warmer at night. Further, when the warmer temperatures were combined with ambient humidity conditions, the composite values consistently revealed even warmer heat-related variables within the urban environment as compared with the rural zone.http://dx.doi.org/10.1155/2010/230365
collection DOAJ
language English
format Article
sources DOAJ
author Jeffrey B. Basara
Heather G. Basara
Bradley G. Illston
Kenneth C. Crawford
spellingShingle Jeffrey B. Basara
Heather G. Basara
Bradley G. Illston
Kenneth C. Crawford
The Impact of the Urban Heat Island during an Intense Heat Wave in Oklahoma City
Advances in Meteorology
author_facet Jeffrey B. Basara
Heather G. Basara
Bradley G. Illston
Kenneth C. Crawford
author_sort Jeffrey B. Basara
title The Impact of the Urban Heat Island during an Intense Heat Wave in Oklahoma City
title_short The Impact of the Urban Heat Island during an Intense Heat Wave in Oklahoma City
title_full The Impact of the Urban Heat Island during an Intense Heat Wave in Oklahoma City
title_fullStr The Impact of the Urban Heat Island during an Intense Heat Wave in Oklahoma City
title_full_unstemmed The Impact of the Urban Heat Island during an Intense Heat Wave in Oklahoma City
title_sort impact of the urban heat island during an intense heat wave in oklahoma city
publisher Hindawi Limited
series Advances in Meteorology
issn 1687-9309
1687-9317
publishDate 2010-01-01
description During late July and early August 2008, an intense heat wave occurred in Oklahoma City. To quantify the impact of the urban heat island (UHI) in Oklahoma City on observed and apparent temperature conditions during the heat wave event, this study used observations from 46 locations in and around Oklahoma City. The methodology utilized composite values of atmospheric conditions for three primary categories defined by population and general land use: rural, suburban, and urban. The results of the analyses demonstrated that a consistent UHI existed during the study period whereby the composite temperature values within the urban core were approximately 0.5∘C warmer during the day than the rural areas and over 2∘C warmer at night. Further, when the warmer temperatures were combined with ambient humidity conditions, the composite values consistently revealed even warmer heat-related variables within the urban environment as compared with the rural zone.
url http://dx.doi.org/10.1155/2010/230365
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