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    Source: Monthly Weather Review:;1987:;volume( 115 ):;issue: 007:;page 1460
    Author(s): Singh, S. V.; Kripalani, R. H.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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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(s): Singh, S. V.; Kripalani, R. H.
    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 ...
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    Potential Predictability of Lower-Tropospheric Monsoon Circulation and Rainfall over India 

    Source: Monthly Weather Review:;1986:;volume( 114 ):;issue: 004:;page 758
    Author(s): Singh, S. V.; Kripalani, R. H.
    Publisher: American Meteorological Society
    Abstract: The potential predictability of the lower tropospheric circulation and the rainfall over India during the peak summer monsoon season (July?August) is studied by analyzing the signal-to-noise ratio. Daily 700-mb heights, ...
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    Interannual Variability of the Madden-Julian Oscillations in Indian Summer Monsoon Rainfall 

    Source: Journal of Climate:;1992:;volume( 005 ):;issue: 009:;page 973
    Author(s): Singh, S. V.; Kripalani, R. H.; Sikka, D. R.
    Publisher: American Meteorological Society
    Abstract: The Madden-Julian oscillations are quite prominent over the Indian monsoon region and they are related with the large-scale active-break phases of the monsoon. These oscillations, however, show considerable inter-annual ...
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    Synoptic Climatology of the Daily 700 mb Summer Monsoon Flow Patterns over India 

    Source: Monthly Weather Review:;1978:;volume( 106 ):;issue: 004:;page 510
    Author(s): Singh, S. V.; Mooley, D. A.; Kripalani, R. H.
    Publisher: American Meteorological Society
    Abstract: The daily (mean of 0000 and 1200 GMT) 700 mb contour patterns over India are classified in five broad types for each summer monsoon month by using a chart-to-chart correlation method. Certain characteristics of these ...
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