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    Response of Meridional Wind to Greenhouse Gas Forcing, Arctic Sea-Ice Loss, and Arctic Amplification

    Source: Journal of Climate:;2022:;volume( 035 ):;issue: 022::page 3675
    Author:
    Xiaodan Chen
    ,
    Aiguo Dai
    DOI: 10.1175/JCLI-D-22-0023.1
    Publisher: American Meteorological Society
    Abstract: Under increasing greenhouse gases, the Arctic warms about twice as fast as elsewhere, known as Arctic amplification (AA). AA weakens meridional temperature gradients and is hypothesized to weaken zonal wind and cause wavier circulation with stronger meridional wind (
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      Response of Meridional Wind to Greenhouse Gas Forcing, Arctic Sea-Ice Loss, and Arctic Amplification

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4290096
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    contributor authorXiaodan Chen
    contributor authorAiguo Dai
    date accessioned2023-04-12T18:42:09Z
    date available2023-04-12T18:42:09Z
    date copyright2022/10/31
    date issued2022
    identifier otherJCLI-D-22-0023.1.pdf
    identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4290096
    description abstractUnder increasing greenhouse gases, the Arctic warms about twice as fast as elsewhere, known as Arctic amplification (AA). AA weakens meridional temperature gradients and is hypothesized to weaken zonal wind and cause wavier circulation with stronger meridional wind (
    publisherAmerican Meteorological Society
    titleResponse of Meridional Wind to Greenhouse Gas Forcing, Arctic Sea-Ice Loss, and Arctic Amplification
    typeJournal Paper
    journal volume35
    journal issue22
    journal titleJournal of Climate
    identifier doi10.1175/JCLI-D-22-0023.1
    journal fristpage3675
    journal lastpage3697
    page3675–3697
    treeJournal of Climate:;2022:;volume( 035 ):;issue: 022
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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