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    The Role of Surface Friction in Tropical Intraseasonal Oscillation

    Source: Monthly Weather Review:;2001:;volume( 129 ):;issue: 004::page 896
    Author:
    Chao, Winston C.
    ,
    Chen, Baode
    DOI: 10.1175/1520-0493(2001)129<0896:TROSFI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The role of surface friction in the tropical intraseasonal oscillation, or the Madden?Julian oscillation (MJO), is investigated by comparing two 4-yr integrations with the Goddard atmospheric general circulation model: one with the original model design with one added feature to enhance the intensity of the MJO and the other is identical but with surface friction in the Tropics replaced by its zonal mean value. This comparison indicates that in the second experiment the MJO not only still exists but also exists with similar intensity. The oft-cited frictional wave-CISK (FWC) interpretation for the origin of the MJO, which emphasizes the role of frictionally induced convergence in the surface layer, is reassessed in light of these experiments. The possibility of the MJO in the second experiment being forced by the middle latitudes is excluded by a third experiment. These experiments do not support one of the central ideas in FWC that surface friction plays an instability-enhancing role.
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      The Role of Surface Friction in Tropical Intraseasonal Oscillation

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4204743
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    contributor authorChao, Winston C.
    contributor authorChen, Baode
    date accessioned2017-06-09T16:13:37Z
    date available2017-06-09T16:13:37Z
    date copyright2001/04/01
    date issued2001
    identifier issn0027-0644
    identifier otherams-63710.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4204743
    description abstractThe role of surface friction in the tropical intraseasonal oscillation, or the Madden?Julian oscillation (MJO), is investigated by comparing two 4-yr integrations with the Goddard atmospheric general circulation model: one with the original model design with one added feature to enhance the intensity of the MJO and the other is identical but with surface friction in the Tropics replaced by its zonal mean value. This comparison indicates that in the second experiment the MJO not only still exists but also exists with similar intensity. The oft-cited frictional wave-CISK (FWC) interpretation for the origin of the MJO, which emphasizes the role of frictionally induced convergence in the surface layer, is reassessed in light of these experiments. The possibility of the MJO in the second experiment being forced by the middle latitudes is excluded by a third experiment. These experiments do not support one of the central ideas in FWC that surface friction plays an instability-enhancing role.
    publisherAmerican Meteorological Society
    titleThe Role of Surface Friction in Tropical Intraseasonal Oscillation
    typeJournal Paper
    journal volume129
    journal issue4
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(2001)129<0896:TROSFI>2.0.CO;2
    journal fristpage896
    journal lastpage904
    treeMonthly Weather Review:;2001:;volume( 129 ):;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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