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Hydrography of the Wadge bank - premonsoon and monsoon seasons
(Indian Association for Limnology and Oceanography, 1989)
The hydrography of the Wadge Bank during premonsoon and monsoon seasons is presented. The thermocline slopes downward towards the central region. Upwelling is prominent in the entire region during monsoon and is observed ...
Latent and sensible heat fluexes under active and weak phases of the summer monsoon of 1986
(Indian Academy of Sciences, Bangalore, 1989)
Summer monsoonal heat balance for upper central equatorial Indian Ocean
(CSIR-NISCAIR, 1989)
Heat budget of the Ocean
(1989)
Variability in wave refraction and resultant nearshore current patterns: Exposed versus sheltered beaches along north Karnataka, west coast of India
(CSIR-NISCAIR, 1988)
For predominant waves approaching from directions varying between SW and WNW and periods varying from 6 to 11 sec, the refraction function (Kd) shows amplification of wave heights resulting in concentration of wave energy ...
Nature of the observed oscillatory flows in shelf waters of the western continental shelf of India
(Tirunelveli: JCSONLINE, 1988)
Time series data on currents obtained from three Aanderaa current meters moored at a station depth of 92 m in the waters of the western continental shelf of India during May 1984 indicated the presence of oscillatory flows. ...
Satellite-tracked drifting buoy observations in the south equatorial current in the Indian Ocean
(Indian Academy of Sciences, Bangalore, 1988)
Three satellite-tracked drifting buoys released in the south equatorial current in the Indian Ocean followed the path of the current moving westward approximately zonally in the vicinity of 10 degrees S latitude. On nearing ...
Shipboard and laboratory equipment
(New Delhi: Department of Ocean Development, 1988)
The polymetallic nodules occur at an average depth of 4500 m. Adequate equipment and techniques are required for the exploration at such depths. Shipboard and various laboratory equipments for the sampling of polymetallic ...
Link node model for the simulation of tides in the Gironde estuary, France
(CSIR-NISCAIR, 1988)