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    ECMWF and ERS-1 Surface Winds over the Arabian Sea during July 1995

    Source: Journal of Physical Oceanography:;1999:;Volume( 029 ):;issue: 007::page 1619
    Author:
    Halpern, David
    ,
    Freilich, Michael H.
    ,
    Weller, Robert A.
    DOI: 10.1175/1520-0485(1999)029<1619:EAESWO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The European Centre for Medium-Range Weather Forecasts (ECMWF) and Institut Francais Pour la Recherche et l?Exploitation de la Mer European Remote-Sensing Satellite, named IFR2, surface wind velocity data products are compared during July 1995 over the Arabian Sea. Substantial differences were found. The central positions of the maximum isotach were separated by 450 km, and the ECMWF maximum isotach was 2 m s?1 higher than that of IFR2. IFR2 wind components contained about 10 times more variance than ECMWF winds for horizontal distances from 50 to 250 km. Along the 8.5°N southern boundary of the Arabian Sea, ECMWF southward Ekman transport was higher than that of IFR2 by an amount that could be observed with current measurements. The ECMWF and IFR2 difference in upward transport of water into the Ekman layer, computed from wind stress curl, was large enough to measure.
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      ECMWF and ERS-1 Surface Winds over the Arabian Sea during July 1995

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4166254
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    • Journal of Physical Oceanography

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    contributor authorHalpern, David
    contributor authorFreilich, Michael H.
    contributor authorWeller, Robert A.
    date accessioned2017-06-09T14:53:33Z
    date available2017-06-09T14:53:33Z
    date copyright1999/07/01
    date issued1999
    identifier issn0022-3670
    identifier otherams-29068.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4166254
    description abstractThe European Centre for Medium-Range Weather Forecasts (ECMWF) and Institut Francais Pour la Recherche et l?Exploitation de la Mer European Remote-Sensing Satellite, named IFR2, surface wind velocity data products are compared during July 1995 over the Arabian Sea. Substantial differences were found. The central positions of the maximum isotach were separated by 450 km, and the ECMWF maximum isotach was 2 m s?1 higher than that of IFR2. IFR2 wind components contained about 10 times more variance than ECMWF winds for horizontal distances from 50 to 250 km. Along the 8.5°N southern boundary of the Arabian Sea, ECMWF southward Ekman transport was higher than that of IFR2 by an amount that could be observed with current measurements. The ECMWF and IFR2 difference in upward transport of water into the Ekman layer, computed from wind stress curl, was large enough to measure.
    publisherAmerican Meteorological Society
    titleECMWF and ERS-1 Surface Winds over the Arabian Sea during July 1995
    typeJournal Paper
    journal volume29
    journal issue7
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1999)029<1619:EAESWO>2.0.CO;2
    journal fristpage1619
    journal lastpage1623
    treeJournal of Physical Oceanography:;1999:;Volume( 029 ):;issue: 007
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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