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    North Atlantic Oscillation Response to Anomalous Indian Ocean SST in a Coupled GCM

    Source: Journal of Climate:;2005:;volume( 018 ):;issue: 024::page 5382
    Author:
    Bader, Jürgen
    ,
    Latif, Mojib
    DOI: 10.1175/JCLI3577.1
    Publisher: American Meteorological Society
    Abstract: The dominant pattern of atmospheric variability in the North Atlantic sector is the North Atlantic Oscillation (NAO). Since the 1970s the NAO has been well characterized by a trend toward its positive phase. Recent atmospheric general circulation model studies have linked this trend to a progressive warming of the Indian Ocean. Unfortunately, a clear mechanism responsible for the change of the NAO could not be given. This study provides further details of the NAO response to Indian Ocean sea surface temperature (SST) anomalies. This is done by conducting experiments with a coupled ocean?atmosphere general circulation model (OAGCM). The authors develop a hypothesis of how the Indian Ocean impacts the NAO.
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      North Atlantic Oscillation Response to Anomalous Indian Ocean SST in a Coupled GCM

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4220676
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    contributor authorBader, Jürgen
    contributor authorLatif, Mojib
    date accessioned2017-06-09T17:01:14Z
    date available2017-06-09T17:01:14Z
    date copyright2005/12/01
    date issued2005
    identifier issn0894-8755
    identifier otherams-78050.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4220676
    description abstractThe dominant pattern of atmospheric variability in the North Atlantic sector is the North Atlantic Oscillation (NAO). Since the 1970s the NAO has been well characterized by a trend toward its positive phase. Recent atmospheric general circulation model studies have linked this trend to a progressive warming of the Indian Ocean. Unfortunately, a clear mechanism responsible for the change of the NAO could not be given. This study provides further details of the NAO response to Indian Ocean sea surface temperature (SST) anomalies. This is done by conducting experiments with a coupled ocean?atmosphere general circulation model (OAGCM). The authors develop a hypothesis of how the Indian Ocean impacts the NAO.
    publisherAmerican Meteorological Society
    titleNorth Atlantic Oscillation Response to Anomalous Indian Ocean SST in a Coupled GCM
    typeJournal Paper
    journal volume18
    journal issue24
    journal titleJournal of Climate
    identifier doi10.1175/JCLI3577.1
    journal fristpage5382
    journal lastpage5389
    treeJournal of Climate:;2005:;volume( 018 ):;issue: 024
    contenttypeFulltext
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