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    Synergistic Interactions between Urban Heat Islands and Heat Waves: The Impact in Cities Is Larger than the Sum of Its Parts

    Source: Journal of Applied Meteorology and Climatology:;2013:;volume( 052 ):;issue: 009::page 2051
    Author:
    Li, Dan
    ,
    Bou-Zeid, Elie
    DOI: 10.1175/JAMC-D-13-02.1
    Publisher: American Meteorological Society
    Abstract: ities are well known to be hotter than the rural areas that surround them; this phenomenon is called the urban heat island. Heat waves are excessively hot periods during which the air temperatures of both urban and rural areas increase significantly. However, whether urban and rural temperatures respond in the same way to heat waves remains a critical unanswered question. In this study, a combination of observational and modeling analyses indicates synergies between urban heat islands and heat waves. That is, not only do heat waves increase the ambient temperatures, but they also intensify the difference between urban and rural temperatures. As a result, the added heat stress in cities will be even higher than the sum of the background urban heat island effect and the heat wave effect. Results presented here also attribute this added impact of heat waves on urban areas to the lack of surface moisture in urban areas and the low wind speed associated with heat waves. Given that heat waves are projected to become more frequent and that urban populations are substantially increasing, these findings underline the serious heat-related health risks facing urban residents in the twenty-first century. Adaptation and mitigation strategies will require joint efforts to reinvent the city, allowing for more green spaces and lesser disruption of the natural water cycle.
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      Synergistic Interactions between Urban Heat Islands and Heat Waves: The Impact in Cities Is Larger than the Sum of Its Parts

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4217181
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    contributor authorLi, Dan
    contributor authorBou-Zeid, Elie
    date accessioned2017-06-09T16:49:51Z
    date available2017-06-09T16:49:51Z
    date copyright2013/09/01
    date issued2013
    identifier issn1558-8424
    identifier otherams-74904.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4217181
    description abstractities are well known to be hotter than the rural areas that surround them; this phenomenon is called the urban heat island. Heat waves are excessively hot periods during which the air temperatures of both urban and rural areas increase significantly. However, whether urban and rural temperatures respond in the same way to heat waves remains a critical unanswered question. In this study, a combination of observational and modeling analyses indicates synergies between urban heat islands and heat waves. That is, not only do heat waves increase the ambient temperatures, but they also intensify the difference between urban and rural temperatures. As a result, the added heat stress in cities will be even higher than the sum of the background urban heat island effect and the heat wave effect. Results presented here also attribute this added impact of heat waves on urban areas to the lack of surface moisture in urban areas and the low wind speed associated with heat waves. Given that heat waves are projected to become more frequent and that urban populations are substantially increasing, these findings underline the serious heat-related health risks facing urban residents in the twenty-first century. Adaptation and mitigation strategies will require joint efforts to reinvent the city, allowing for more green spaces and lesser disruption of the natural water cycle.
    publisherAmerican Meteorological Society
    titleSynergistic Interactions between Urban Heat Islands and Heat Waves: The Impact in Cities Is Larger than the Sum of Its Parts
    typeJournal Paper
    journal volume52
    journal issue9
    journal titleJournal of Applied Meteorology and Climatology
    identifier doi10.1175/JAMC-D-13-02.1
    journal fristpage2051
    journal lastpage2064
    treeJournal of Applied Meteorology and Climatology:;2013:;volume( 052 ):;issue: 009
    contenttypeFulltext
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