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Dynamics of the east India coastal current. 1. Analytic solutions forced by interior Ekman pumping and local alongshore winds
(American Geophysical Union, 1996)
On the sea surface temperature high in the Lakshadweep Sea before the onset of the southwest monsoon
(American Geophysical Union, 1999)
The north Indian Ocean becomes the warmest area of the world oceans prior to the onset of southwest monsoon in June. During this period a zonal band of high sea surface temperature (SST), the ``thermal equator'' (TE), moves ...
Dynamics of the east India coastal current. 2. Numerical solutions
(American Geophysical Union, 1996)
A linear, continuously stratified model is used to investigate the dynamics of the East India Coastal Current (EICC). Solutions are found numerically in a basin that resembles the Indian Ocean basin north of 29 degrees S, ...
On the dynamics of the Lakshadweep high and low in the southeastern Arabian Sea
(American Geophysical Union, 1997)
Hydrography and altimetry show that a "high" in surface topography forms off southwest India in January (midnortheast monsoon) and that a "low" forms during the southwest monsoon; the high and low, called Lakshadweep high ...
Are interdecadal sea level changes along the Indian coast influenced by variability of monsoon rainfall?
(American Geophysical Union, 1999)
The Mumbai (Bombay) tide gauge data, the only century-long record in the Indian Ocean, show that interdecadal changes in sea level mimic those in rainfall over the Indian subcontinent. We propose that the link between ...
Sea level during storm surges as seen in tide-gauge records along the east coast of India
(Indian Academy of Sciences, 1999)
Analysis of hourly sea level recorded by tide gauges of the Survey of India (SOI) at Paradip, Vishakhapatnam, and Chennai provides a record of non-tidal sea level during three periods, 6-10 August 1979, 6-10 August 1981, ...
Hydrography and circulation in the western Bay of Bengal during the northeast monsoon
(American Geophysical Union, 1996)
The Bay of Bengal, a semienclosed tropical basin that comes under the influence of monsoonal wind and freshwater influx, is distinguished by a strongly stratified surface layer and a seasonally reversing circulation. We ...