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    The Influence of the Ocean on Typhoon Nuri (2008)

    Source: Monthly Weather Review:;2015:;volume( 143 ):;issue: 011::page 4493
    Author:
    Sun, Jingru
    ,
    Oey, Lie-Yauw
    DOI: 10.1175/MWR-D-15-0029.1
    Publisher: American Meteorological Society
    Abstract: yphoon Nuri (2008) was 1 of approximately 120 typhoons in the past 60 years that passed through a narrow gap, the Luzon Strait, connecting the western North Pacific and the South China Sea (SCS). In total 70% of these storms, including Nuri, reached their maximum intensities over the warm waters east of Luzon and in the Kuroshio, then rapidly weakened in the SCS. Numerical experiments were conducted to understand the intensity change of Nuri. Westward across the Kuroshio in the Luzon Strait, the 26°C isotherm shallows rapidly by half. This and stronger mixing by wind?ocean resonance preferentially cooled sea surface temperature and weakened the typhoon in SCS. A positive-feedback mechanism is then described to explain the intensification of Nuri over the western North Pacific.
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      The Influence of the Ocean on Typhoon Nuri (2008)

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4230709
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    contributor authorSun, Jingru
    contributor authorOey, Lie-Yauw
    date accessioned2017-06-09T17:32:58Z
    date available2017-06-09T17:32:58Z
    date copyright2015/11/01
    date issued2015
    identifier issn0027-0644
    identifier otherams-87080.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4230709
    description abstractyphoon Nuri (2008) was 1 of approximately 120 typhoons in the past 60 years that passed through a narrow gap, the Luzon Strait, connecting the western North Pacific and the South China Sea (SCS). In total 70% of these storms, including Nuri, reached their maximum intensities over the warm waters east of Luzon and in the Kuroshio, then rapidly weakened in the SCS. Numerical experiments were conducted to understand the intensity change of Nuri. Westward across the Kuroshio in the Luzon Strait, the 26°C isotherm shallows rapidly by half. This and stronger mixing by wind?ocean resonance preferentially cooled sea surface temperature and weakened the typhoon in SCS. A positive-feedback mechanism is then described to explain the intensification of Nuri over the western North Pacific.
    publisherAmerican Meteorological Society
    titleThe Influence of the Ocean on Typhoon Nuri (2008)
    typeJournal Paper
    journal volume143
    journal issue11
    journal titleMonthly Weather Review
    identifier doi10.1175/MWR-D-15-0029.1
    journal fristpage4493
    journal lastpage4513
    treeMonthly Weather Review:;2015:;volume( 143 ):;issue: 011
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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