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Now showing items 11-20 of 25

Heat energy exchange over a large water body under stable atmospheric conditions

Sadhuram, Y.; Vethamony, P.; Suryanarayana, A.; Swamy, G.N.; Sastry, J.S. (Kluwer, 1988)

Estimation of evaporation rates over the Arabian Sea from Satellite data

Rao, M.V.; RameshBabu, V.; Rao, L.V.G.; Sastry, J.S. (Indian Academy of Sciences, Bangalore, 1986)

Utilizing both the SAMIR brightness temperatures of Bhaskara 2 and GOSSTCOMP charts of NOAA satellite series, the evaporation rates over the Arabian Sea for June 1982 are estimated through the bulk aerodynamic method. The ...

Watermass structure in the western Indian Ocean - Part 2. The spreading and transformation of the Persian Gulf water

Premchand, K.; Sastry, J.S.; Murty, C.S. (India Meteorological Department, 1986)

The spreading and the transformation of the Persian Gulf Watermass (PGW) in the Arabian Sea and the Indian Ocean have been presented. The core layer of this watermass is found in the depth range of 250-300 m over most of ...

On the characteristics of multipeaked spectra of ocean surface waves

Vethamony, P.; Sastry, J.S. (Institute of Engineers�, 1986)

Surface circulation over the shelf off the east coast of India during the south west monsoon

Gopalakrishna, V.V.; Sastry, J.S. (CSIR-NISCAIR, 1985)

From the hydrographic data collected on board R V Gaveshani in the Western Bay of Bengal during August-September 1978, fields of temperature, salinity have been constructed and the probable flow regime has been deduced. ...

Summer cooling in the east central Arabian Sea - a process of dynamic response to the southwest monsoon

RameshBabu, V.; Sastry, J.S. (India Meteorological Department, 1984)

The cooling of the east central Arabian Sea during summer monsoon season is examined using data sets of MONEX '79 and MONSOON '77 programmes. These studies have revealed that downward transfer of heat due to the mixing of ...

A Comparative Study of Vertical Stabilities in the Arabian Sea and Bay of Bengal

Sastry, J.S.; Rao, D.P. (India Meteorological Department, 1981)

Stabilities in the upper 300 m in the Arabian Sea and the Bay of Bengal are computed and presented seasonwise. The water column in the Bay of Bengal is more strongly stratified than that in the Arabian Sea. These studies ...

Circulation and Distribution of some Hydrographical Properties during the late Winter in the Bay of Bengal

Rao, D.P.; Sastry, J.S. (Indian Association for Limnology and Oceanography, 1981)

Charts showing dynamic topography, mass distribution, temperature, salinity, dissolved oxygen and inorganic phosphate in the upper layers of the Bay of Bengal for the late winter period were analysed and presented. The ...

Shoreline Defromations in Relation to Shore Protection Structures along Kerala Coast

Murty, C.S.; Sastry, J.S.; Varadachari, V.V.R. (CSIR-NISCAIR, 1980)

Beach Morphological Variations over Micro-Time Scales

Murty, C.S.; Veerayya, M.; Sastry, J.S.; Varadachari, V.V.R. (CSIR-NISCAIR, 1980)

Nature and magnitude of beach changes over short periods have been studied at Calangute and Miramar in relation to tide, ground water level and relevant oceanographic and meteorological factors. Alternating zones of accretion ...