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    Rapid Oceanic Response to Tropical Cyclone Oli (2010) over the South Pacific

    Source: Journal of Physical Oceanography:;2017:;Volume( 047 ):;issue: 002::page 471
    Author:
    Oruba, Ludivine
    ,
    Planes, Serge
    ,
    Siu, Gilles
    ,
    Chancerelle, Yannick
    ,
    Dormy, Emmanuel
    DOI: 10.1175/JPO-D-16-0205.1
    Publisher: American Meteorological Society
    Abstract: he effect of Tropical Cyclone Oli (2010) on the ocean is investigated using a variety of measurements. In situ temperature measurements on the cyclone track are available via the Centre de Recherches Insulaires et Observatoire de l?Environnement (CRIOBE) array of probes. This reflects an extreme fluctuation of the temperature some 18 h after the cyclone, lasting only 12 h and exceeding 3°C in amplitude. This study interprets this extreme fluctuation in terms of enhanced mixing associated with the time-dependent inertial currents due to the cyclonic winds. The authors show, using Lagrangian simulations, that this rapid event is compatible with the severe length-scale shortening observed in Lagrangian simulations.
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      Rapid Oceanic Response to Tropical Cyclone Oli (2010) over the South Pacific

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4227292
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    contributor authorOruba, Ludivine
    contributor authorPlanes, Serge
    contributor authorSiu, Gilles
    contributor authorChancerelle, Yannick
    contributor authorDormy, Emmanuel
    date accessioned2017-06-09T17:22:25Z
    date available2017-06-09T17:22:25Z
    date copyright2017/02/01
    date issued2017
    identifier issn0022-3670
    identifier otherams-84003.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4227292
    description abstracthe effect of Tropical Cyclone Oli (2010) on the ocean is investigated using a variety of measurements. In situ temperature measurements on the cyclone track are available via the Centre de Recherches Insulaires et Observatoire de l?Environnement (CRIOBE) array of probes. This reflects an extreme fluctuation of the temperature some 18 h after the cyclone, lasting only 12 h and exceeding 3°C in amplitude. This study interprets this extreme fluctuation in terms of enhanced mixing associated with the time-dependent inertial currents due to the cyclonic winds. The authors show, using Lagrangian simulations, that this rapid event is compatible with the severe length-scale shortening observed in Lagrangian simulations.
    publisherAmerican Meteorological Society
    titleRapid Oceanic Response to Tropical Cyclone Oli (2010) over the South Pacific
    typeJournal Paper
    journal volume47
    journal issue2
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/JPO-D-16-0205.1
    journal fristpage471
    journal lastpage483
    treeJournal of Physical Oceanography:;2017:;Volume( 047 ):;issue: 002
    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
    yabeshDSpacePersian