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    Impacts of the Decadal Urbanization on Thermally Induced Circulations in Eastern China

    Source: Journal of Applied Meteorology and Climatology:;2014:;volume( 054 ):;issue: 002::page 259
    Author:
    Li, Mengmeng
    ,
    Mao, Zhichun
    ,
    Song, Yu
    ,
    Liu, Mingxu
    ,
    Huang, Xin
    DOI: 10.1175/JAMC-D-14-0176.1
    Publisher: American Meteorological Society
    Abstract: ignificant urbanization has occurred in the Yangtze River Delta region of eastern China, which exerts important effects on the local thermally induced circulations through regulating the heat flux and thermal structure. Previous studies lack a correct representation of the seasonal vegetation phenology associated with urban expansion, and therefore it is difficult to accurately describe the land?atmosphere coupling. In this study, high-resolution Moderate Resolution Imaging Spectroradiometer (MODIS) observations are used to describe the changes in land surface characteristics, including land-cover type, green vegetation fraction, and leaf area index with the Weather Research and Forecasting Model. The use of MODIS satellite observations provides a clear improvement in model performance when compared with ground-based measurements. A typical urban heat island is generated around Shanghai, Wuxi?Suzhou?Yangzhou, and cities along the Yangtze River and Hangzhou Bay, which subsequently modifies the local thermal circulations. The sea breeze is significantly enhanced over the north bank of Hangzhou Bay because of the increased land?sea temperature contrast. Several surface convergent zones are generated along the Shanghai?Suzhou?Wuxi city belt as a result of the combined effects of the urban heat island, the enhanced sea breeze, and the lake breeze at Lake Tai.
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      Impacts of the Decadal Urbanization on Thermally Induced Circulations in Eastern China

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    contributor authorLi, Mengmeng
    contributor authorMao, Zhichun
    contributor authorSong, Yu
    contributor authorLiu, Mingxu
    contributor authorHuang, Xin
    date accessioned2017-06-09T16:50:31Z
    date available2017-06-09T16:50:31Z
    date copyright2015/02/01
    date issued2014
    identifier issn1558-8424
    identifier otherams-75103.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4217403
    description abstractignificant urbanization has occurred in the Yangtze River Delta region of eastern China, which exerts important effects on the local thermally induced circulations through regulating the heat flux and thermal structure. Previous studies lack a correct representation of the seasonal vegetation phenology associated with urban expansion, and therefore it is difficult to accurately describe the land?atmosphere coupling. In this study, high-resolution Moderate Resolution Imaging Spectroradiometer (MODIS) observations are used to describe the changes in land surface characteristics, including land-cover type, green vegetation fraction, and leaf area index with the Weather Research and Forecasting Model. The use of MODIS satellite observations provides a clear improvement in model performance when compared with ground-based measurements. A typical urban heat island is generated around Shanghai, Wuxi?Suzhou?Yangzhou, and cities along the Yangtze River and Hangzhou Bay, which subsequently modifies the local thermal circulations. The sea breeze is significantly enhanced over the north bank of Hangzhou Bay because of the increased land?sea temperature contrast. Several surface convergent zones are generated along the Shanghai?Suzhou?Wuxi city belt as a result of the combined effects of the urban heat island, the enhanced sea breeze, and the lake breeze at Lake Tai.
    publisherAmerican Meteorological Society
    titleImpacts of the Decadal Urbanization on Thermally Induced Circulations in Eastern China
    typeJournal Paper
    journal volume54
    journal issue2
    journal titleJournal of Applied Meteorology and Climatology
    identifier doi10.1175/JAMC-D-14-0176.1
    journal fristpage259
    journal lastpage282
    treeJournal of Applied Meteorology and Climatology:;2014:;volume( 054 ):;issue: 002
    contenttypeFulltext
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