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Studies on thermal fields in the Bay of Bengal
(Indian Geological Congress, Roorkee, India, 2000)
As an Indian component of the International Tropical Ocean Global Atmosphere (TOGA) program, the National Institute of Oceanography, Goa, has initiated a long-term observational program during 1990 with financial support ...
Sediment dispersal during ne monsoon over northern Bay of Bengal: Preliminary results using IRS-P4 OCM data
(NIO, Dona Paula, Goa (India), 2000)
False Color Composite (FCC) from the sequential satellite images of Indian Remote Sensing Satellite IRS-P4 OCM (bands around 443, 555, and 845 nm) together with sea truth data acquisition at 42 stations along the Orissa ...
Wave climatology of the Indian Ocean derived from altimetry and wave model
(NIO, Dona Paula, Goa (India), 2000)
GEOSAT altimeter data for the period 1986-1989 have been utilised to derive wave climatology for the Indian Ocean region bounded by 20 degrees S to 25 degrees N and 40 degrees E to 110 degrees E. The results are presented ...
Anomalous circulation in the eastern equatorial Indian Ocean during southwest monsoon of 1994
(NIO, Dona Paula, Goa (India), 2000)
Geostrophic circulation derived from hydrographic data collected during July-August, 1994 along 80, 84 and 88E between 5N and 3S latitudinal belt in the eastern equatorial Indian Ocean is presented. A broad westward flow ...
Upwelling and associated hydrography along the west coast of india during southwest monsoon, 1999
(NIO, Dona Paula, Goa (India), 2000)
During May 1999 twenty-five hydrographic stations were carried out covering the waters of the west coast of India from 8 degrees N to 13 degrees N as a part of Marine Research - Living Resources (MR-LR) programme. The ...
Hydrological structure and biological productivity of the tropical Indian Ocean
(NIO, Dona Paula, Goa (India), 2000)
Hydrological structure analyses of regions in the tropical Atlantic Ocean have consistently revealed the existence of a typical tropical structure characterized by a nitrate-depleted mixed layer above the thermocline. The ...