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    Tropical Atmospheric Variability Forced by Oceanic Internal Variability

    Source: Journal of Climate:;2007:;volume( 020 ):;issue: 004::page 765
    Author:
    Jochum, Markus
    ,
    Deser, Clara
    ,
    Phillips, Adam
    DOI: 10.1175/JCLI4044.1
    Publisher: American Meteorological Society
    Abstract: Atmospheric general circulation model experiments are conducted to quantify the contribution of internal oceanic variability in the form of tropical instability waves (TIWs) to interannual wind and rainfall variability in the tropical Pacific. It is found that in the tropical Pacific, along the equator, and near 25°N and 25°S, TIWs force a significant increase in wind and rainfall variability from interseasonal to interannual time scales. Because of the stochastic nature of TIWs, this means that climate models that do not take them into account will underestimate the strength and number of extreme events and may overestimate forecast capability.
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      Tropical Atmospheric Variability Forced by Oceanic Internal Variability

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4221184
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    contributor authorJochum, Markus
    contributor authorDeser, Clara
    contributor authorPhillips, Adam
    date accessioned2017-06-09T17:02:53Z
    date available2017-06-09T17:02:53Z
    date copyright2007/02/01
    date issued2007
    identifier issn0894-8755
    identifier otherams-78507.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4221184
    description abstractAtmospheric general circulation model experiments are conducted to quantify the contribution of internal oceanic variability in the form of tropical instability waves (TIWs) to interannual wind and rainfall variability in the tropical Pacific. It is found that in the tropical Pacific, along the equator, and near 25°N and 25°S, TIWs force a significant increase in wind and rainfall variability from interseasonal to interannual time scales. Because of the stochastic nature of TIWs, this means that climate models that do not take them into account will underestimate the strength and number of extreme events and may overestimate forecast capability.
    publisherAmerican Meteorological Society
    titleTropical Atmospheric Variability Forced by Oceanic Internal Variability
    typeJournal Paper
    journal volume20
    journal issue4
    journal titleJournal of Climate
    identifier doi10.1175/JCLI4044.1
    journal fristpage765
    journal lastpage771
    treeJournal of Climate:;2007:;volume( 020 ):;issue: 004
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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