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    Summer-to-Winter Sea-Ice Linkage between the Arctic Ocean and the Okhotsk Sea through Atmospheric Circulation

    Source: Journal of Climate:;2015:;volume( 028 ):;issue: 012::page 4971
    Author:
    Ogi, Masayo
    ,
    Taguchi, Bunmei
    ,
    Honda, Meiji
    ,
    Barber, David G.
    ,
    Rysgaard, Søren
    DOI: 10.1175/JCLI-D-14-00297.1
    Publisher: American Meteorological Society
    Abstract: ontemporary climate science seeks to understand the rate and magnitude of a warming global climate and how it impacts regional variability and teleconnections. One of the key drivers of regional climate is the observed reduction in end of summer sea-ice extent over the Arctic. Here the authors show that interannual variations between the September Arctic sea-ice concentration, especially in the East Siberian Sea, and the maximum Okhotsk sea-ice extent in the following winter are positively correlated, which is not explained by the recent warming trend only. An increase of sea ice both in the East Siberian Sea and the Okhotsk Sea and corresponding atmospheric patterns, showing a seesaw between positive anomalies of sea level pressures over the Arctic Ocean and negative anomalies over the midlatitudes, are related to cold anomalies over the high-latitude Eurasian continent. The patterns of atmospheric circulation and air temperatures are similar to those of the annually integrated Arctic Oscillation (AO). The negative annual AO forms colder anomalies in autumn sea surface temperatures both over the East Siberian Sea and the Okhotsk Sea, which causes heavy sea-ice conditions in both seas through season-to-season persistence.
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      Summer-to-Winter Sea-Ice Linkage between the Arctic Ocean and the Okhotsk Sea through Atmospheric Circulation

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4223490
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    contributor authorOgi, Masayo
    contributor authorTaguchi, Bunmei
    contributor authorHonda, Meiji
    contributor authorBarber, David G.
    contributor authorRysgaard, Søren
    date accessioned2017-06-09T17:10:32Z
    date available2017-06-09T17:10:32Z
    date copyright2015/06/01
    date issued2015
    identifier issn0894-8755
    identifier otherams-80582.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4223490
    description abstractontemporary climate science seeks to understand the rate and magnitude of a warming global climate and how it impacts regional variability and teleconnections. One of the key drivers of regional climate is the observed reduction in end of summer sea-ice extent over the Arctic. Here the authors show that interannual variations between the September Arctic sea-ice concentration, especially in the East Siberian Sea, and the maximum Okhotsk sea-ice extent in the following winter are positively correlated, which is not explained by the recent warming trend only. An increase of sea ice both in the East Siberian Sea and the Okhotsk Sea and corresponding atmospheric patterns, showing a seesaw between positive anomalies of sea level pressures over the Arctic Ocean and negative anomalies over the midlatitudes, are related to cold anomalies over the high-latitude Eurasian continent. The patterns of atmospheric circulation and air temperatures are similar to those of the annually integrated Arctic Oscillation (AO). The negative annual AO forms colder anomalies in autumn sea surface temperatures both over the East Siberian Sea and the Okhotsk Sea, which causes heavy sea-ice conditions in both seas through season-to-season persistence.
    publisherAmerican Meteorological Society
    titleSummer-to-Winter Sea-Ice Linkage between the Arctic Ocean and the Okhotsk Sea through Atmospheric Circulation
    typeJournal Paper
    journal volume28
    journal issue12
    journal titleJournal of Climate
    identifier doi10.1175/JCLI-D-14-00297.1
    journal fristpage4971
    journal lastpage4979
    treeJournal of Climate:;2015:;volume( 028 ):;issue: 012
    contenttypeFulltext
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