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    Global Climate Variations Connected with Sea Surface Temperature Anomalies in the Eastern Equatorial Pacific Ocean for the 1958–73 Period

    Source: Monthly Weather Review:;1983:;volume( 111 ):;issue: 006::page 1244
    Author:
    Pan, Yi Hong
    ,
    Oort, Abraham H.
    DOI: 10.1175/1520-0493(1983)111<1244:GCVCWS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The sea surface temperature anomalies in the eastern equatorial Pacific Ocean are shown to demarcate a ?key region? new 130°W for observed variations in the global general circulation. Various techniques are used to describe global conditions during warm and cold sea surface conditions in the key region based on a global 15-year set of surface and upper air analyses. Earlier work is confirmed that during warm episodes 1) the westerly jets in both hemispheres are strengthened, and 2) some of the semi-permanent circulation features, such as the intertropical convergence zone, the subtropical high over the western and central Pacific, and the Aleutian low, increase in strength, and vice versa for cold episodes. The time series of monthly-mean atmospheric temperature averaged over the entire man of the Northern Hemisphere is found to be highly correlated with the sea surface temperature anomalies in the key region. The highest correlation of r = 0.65 is found when the atmosphere lags the ocean by 6 months. The maximum temperature response seems to occur in the upper troposphere in the tropics probably associated with variations in convective activity.
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      Global Climate Variations Connected with Sea Surface Temperature Anomalies in the Eastern Equatorial Pacific Ocean for the 1958–73 Period

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4200924
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    • Monthly Weather Review

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    contributor authorPan, Yi Hong
    contributor authorOort, Abraham H.
    date accessioned2017-06-09T16:04:24Z
    date available2017-06-09T16:04:24Z
    date copyright1983/06/01
    date issued1983
    identifier issn0027-0644
    identifier otherams-60272.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4200924
    description abstractThe sea surface temperature anomalies in the eastern equatorial Pacific Ocean are shown to demarcate a ?key region? new 130°W for observed variations in the global general circulation. Various techniques are used to describe global conditions during warm and cold sea surface conditions in the key region based on a global 15-year set of surface and upper air analyses. Earlier work is confirmed that during warm episodes 1) the westerly jets in both hemispheres are strengthened, and 2) some of the semi-permanent circulation features, such as the intertropical convergence zone, the subtropical high over the western and central Pacific, and the Aleutian low, increase in strength, and vice versa for cold episodes. The time series of monthly-mean atmospheric temperature averaged over the entire man of the Northern Hemisphere is found to be highly correlated with the sea surface temperature anomalies in the key region. The highest correlation of r = 0.65 is found when the atmosphere lags the ocean by 6 months. The maximum temperature response seems to occur in the upper troposphere in the tropics probably associated with variations in convective activity.
    publisherAmerican Meteorological Society
    titleGlobal Climate Variations Connected with Sea Surface Temperature Anomalies in the Eastern Equatorial Pacific Ocean for the 1958–73 Period
    typeJournal Paper
    journal volume111
    journal issue6
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1983)111<1244:GCVCWS>2.0.CO;2
    journal fristpage1244
    journal lastpage1258
    treeMonthly Weather Review:;1983:;volume( 111 ):;issue: 006
    contenttypeFulltext
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