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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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