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    Measurement of Air–Sea Fluxes over the Indian Ocean and the Bay of Bengal

    Source: Journal of Climate:;2003:;volume( 016 ):;issue: 004::page 767
    Author:
    Bhat, G. S.
    DOI: 10.1175/1520-0442(2003)016<0767:MOASFO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Atmospheric and oceanic data were collected in 1998 and 1999 over the tropical Indian Ocean during three cruises of the Indian research vessel Sagar Kanya, covering different geographic locations and seasons, including boreal winter, peak monsoon, and postmonsoon periods. The present study is mainly based on the measurements made during the three cruises. It is found that there are important differences in the near-surface characteristics during monsoon and other seasons. The largest variations in the net surface heat flux occurred during the monsoon period. The specific humidity difference between sea surface and air at 10-m height shows a strong seasonal dependence, with the lowest values observed during the monsoon period. An important finding from the ship observations is that, at a given SST, the surface air over the Indian Ocean is much warmer compared to that over other tropical oceans and the west Pacific warm pool in particular. These findings are supported by data obtained by a moored buoy in the north Indian Ocean and also from the Comprehensive Ocean?Atmosphere Data Set for the Indian Ocean.
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      Measurement of Air–Sea Fluxes over the Indian Ocean and the Bay of Bengal

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4203412
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    contributor authorBhat, G. S.
    date accessioned2017-06-09T16:10:15Z
    date available2017-06-09T16:10:15Z
    date copyright2003/02/01
    date issued2003
    identifier issn0894-8755
    identifier otherams-6251.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4203412
    description abstractAtmospheric and oceanic data were collected in 1998 and 1999 over the tropical Indian Ocean during three cruises of the Indian research vessel Sagar Kanya, covering different geographic locations and seasons, including boreal winter, peak monsoon, and postmonsoon periods. The present study is mainly based on the measurements made during the three cruises. It is found that there are important differences in the near-surface characteristics during monsoon and other seasons. The largest variations in the net surface heat flux occurred during the monsoon period. The specific humidity difference between sea surface and air at 10-m height shows a strong seasonal dependence, with the lowest values observed during the monsoon period. An important finding from the ship observations is that, at a given SST, the surface air over the Indian Ocean is much warmer compared to that over other tropical oceans and the west Pacific warm pool in particular. These findings are supported by data obtained by a moored buoy in the north Indian Ocean and also from the Comprehensive Ocean?Atmosphere Data Set for the Indian Ocean.
    publisherAmerican Meteorological Society
    titleMeasurement of Air–Sea Fluxes over the Indian Ocean and the Bay of Bengal
    typeJournal Paper
    journal volume16
    journal issue4
    journal titleJournal of Climate
    identifier doi10.1175/1520-0442(2003)016<0767:MOASFO>2.0.CO;2
    journal fristpage767
    journal lastpage775
    treeJournal of Climate:;2003:;volume( 016 ):;issue: 004
    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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