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    MONTHLY CHARTS OF SURFACE WIND STRESS CURL OVER THE INDIAN OCEAN

    Source: Monthly Weather Review:;1970:;volume( 098 ):;issue: 010::page 765
    Author:
    HANTEL, MICHAEL
    DOI: 10.1175/1520-0493(1970)098<0765:MCOSWS>2.3.CO;2
    Publisher: American Meteorological Society
    Abstract: The surface wind stress curl is the forcing function in the equations of vertically integrated water transport of wind-driven ocean currents. Hence, it has become a basic quantity in theoretical oceanography. As the time dependence of all important surface quantities in the Indian Ocean is stronger than in other oceans, it is valuable to look particularly at the time variation in this region. This study presents monthly charts of the wind stress curl at the surface of the Indian Ocean from its land boundaries up to 50° S. and from 20° E. to 116° E. Basic data were the monthly surface maps of the Koninklijk Nederlands Meteorologisch Instituut, derived from ship observations and given as 2° square means of the surface wind. The processing of the data is described in detail. In particular, small-scale fluctuations are objectively filtered out. While earlier compilations are usually on a coarser grid (seasonal and 5° square averages), the present data have a refined time and space resolution. Therefore, they allow one to study more detailed structures. In particular, the charts show that the curl pattern in the Indian Ocean is not independent of longitude.
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      MONTHLY CHARTS OF SURFACE WIND STRESS CURL OVER THE INDIAN OCEAN

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4198682
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    • Monthly Weather Review

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    contributor authorHANTEL, MICHAEL
    date accessioned2017-06-09T15:59:26Z
    date available2017-06-09T15:59:26Z
    date copyright1970/10/01
    date issued1970
    identifier issn0027-0644
    identifier otherams-58255.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4198682
    description abstractThe surface wind stress curl is the forcing function in the equations of vertically integrated water transport of wind-driven ocean currents. Hence, it has become a basic quantity in theoretical oceanography. As the time dependence of all important surface quantities in the Indian Ocean is stronger than in other oceans, it is valuable to look particularly at the time variation in this region. This study presents monthly charts of the wind stress curl at the surface of the Indian Ocean from its land boundaries up to 50° S. and from 20° E. to 116° E. Basic data were the monthly surface maps of the Koninklijk Nederlands Meteorologisch Instituut, derived from ship observations and given as 2° square means of the surface wind. The processing of the data is described in detail. In particular, small-scale fluctuations are objectively filtered out. While earlier compilations are usually on a coarser grid (seasonal and 5° square averages), the present data have a refined time and space resolution. Therefore, they allow one to study more detailed structures. In particular, the charts show that the curl pattern in the Indian Ocean is not independent of longitude.
    publisherAmerican Meteorological Society
    titleMONTHLY CHARTS OF SURFACE WIND STRESS CURL OVER THE INDIAN OCEAN
    typeJournal Paper
    journal volume98
    journal issue10
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1970)098<0765:MCOSWS>2.3.CO;2
    journal fristpage765
    journal lastpage773
    treeMonthly Weather Review:;1970:;volume( 098 ):;issue: 010
    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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