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    Teleconnections from Tropics to Northern Extratropics through a Southerly Conveyor

    Source: Journal of the Atmospheric Sciences:;2005:;Volume( 062 ):;issue: 011::page 4057
    Author:
    Wang, Zhuo
    ,
    Chang, C-P.
    ,
    Wang, Bin
    ,
    Jin, Fei-Fei
    DOI: 10.1175/JAS3600.1
    Publisher: American Meteorological Society
    Abstract: Rossby wave propagation theory predicts that Rossby waves in a tropical easterly flow cannot escape from the Tropics to the extratropics. Here the authors show that a southerly flow component in the basic state (a southerly conveyor) may transfer a Rossby wave source northward; thus, a forcing embedded in the deep tropical easterlies may excite a Rossby wave response in the extratropical westerlies. It is shown that the southerly conveyor determines the location of the effective Rossby wave source and that the extratropical response is relatively insensitive to the location of the tropical forcing, provided that the tropical response can reach the southerly conveyor. A stronger southerly flow favors a stronger extratropical response, and the spatial structure of the extratropical response is determined by the extratropical westerly basic flows.
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      Teleconnections from Tropics to Northern Extratropics through a Southerly Conveyor

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4218161
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    contributor authorWang, Zhuo
    contributor authorChang, C-P.
    contributor authorWang, Bin
    contributor authorJin, Fei-Fei
    date accessioned2017-06-09T16:52:37Z
    date available2017-06-09T16:52:37Z
    date copyright2005/11/01
    date issued2005
    identifier issn0022-4928
    identifier otherams-75787.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4218161
    description abstractRossby wave propagation theory predicts that Rossby waves in a tropical easterly flow cannot escape from the Tropics to the extratropics. Here the authors show that a southerly flow component in the basic state (a southerly conveyor) may transfer a Rossby wave source northward; thus, a forcing embedded in the deep tropical easterlies may excite a Rossby wave response in the extratropical westerlies. It is shown that the southerly conveyor determines the location of the effective Rossby wave source and that the extratropical response is relatively insensitive to the location of the tropical forcing, provided that the tropical response can reach the southerly conveyor. A stronger southerly flow favors a stronger extratropical response, and the spatial structure of the extratropical response is determined by the extratropical westerly basic flows.
    publisherAmerican Meteorological Society
    titleTeleconnections from Tropics to Northern Extratropics through a Southerly Conveyor
    typeJournal Paper
    journal volume62
    journal issue11
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/JAS3600.1
    journal fristpage4057
    journal lastpage4070
    treeJournal of the Atmospheric Sciences:;2005:;Volume( 062 ):;issue: 011
    contenttypeFulltext
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