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    Application of Extended Empirical Orthogonal Function Analysis to Interrelationships and Sequential Evolution of Monsoon Fields

    Source: Monthly Weather Review:;1986:;volume( 114 ):;issue: 008::page 1603
    Author:
    Singh, S. V.
    ,
    Kripalani, R. H.
    DOI: 10.1175/1520-0493(1986)114<1603:AOEEOF>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Extended empirical orthogonal function (EEOF) analysis has been employed to study linear relationships among the mean sea level pressure, 700 mb height and rainfall over India, and their low-frequency sequential evolution during the peak summer monsoon months. The interrelationships between these fields are strongest over central India and, while the rainfall activity is colocated with the corresponding changes in the 700 mb heights, it is displaced southward with respect to the pressure changes. The first two EEOF's of all the three fields (averaged over 5 or 7 days) show that the dominant low-frequency sequential evolution is associated with north and northeastward movement of the anomaly centers with a recurrence period of about 40 days. In addition, the presence of a westward moving wave in sea level pressure anomalies located roughly near 15°N latitude is revealed by the third EEOF.
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      Application of Extended Empirical Orthogonal Function Analysis to Interrelationships and Sequential Evolution of Monsoon Fields

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4201591
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    • Monthly Weather Review

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    contributor authorSingh, S. V.
    contributor authorKripalani, R. H.
    date accessioned2017-06-09T16:05:54Z
    date available2017-06-09T16:05:54Z
    date copyright1986/08/01
    date issued1986
    identifier issn0027-0644
    identifier otherams-60873.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4201591
    description abstractExtended empirical orthogonal function (EEOF) analysis has been employed to study linear relationships among the mean sea level pressure, 700 mb height and rainfall over India, and their low-frequency sequential evolution during the peak summer monsoon months. The interrelationships between these fields are strongest over central India and, while the rainfall activity is colocated with the corresponding changes in the 700 mb heights, it is displaced southward with respect to the pressure changes. The first two EEOF's of all the three fields (averaged over 5 or 7 days) show that the dominant low-frequency sequential evolution is associated with north and northeastward movement of the anomaly centers with a recurrence period of about 40 days. In addition, the presence of a westward moving wave in sea level pressure anomalies located roughly near 15°N latitude is revealed by the third EEOF.
    publisherAmerican Meteorological Society
    titleApplication of Extended Empirical Orthogonal Function Analysis to Interrelationships and Sequential Evolution of Monsoon Fields
    typeJournal Paper
    journal volume114
    journal issue8
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1986)114<1603:AOEEOF>2.0.CO;2
    journal fristpage1603
    journal lastpage1611
    treeMonthly Weather Review:;1986:;volume( 114 ):;issue: 008
    contenttypeFulltext
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