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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 ...
Apparent relationship between thermal regime in Antarctic waters and Indian summer monsoon
(CSIR-NISCAIR, 1988)
Austral winter seasonal and intra-seasonal variabilities of Sub-Tropical Convergence and Antarctic Polar Front are examined using sea surface temperature patterns published in GOSSTCOMP (Global Operational Sea Surface ...
Water characteristics and transport of the Antarctic circumpolar current in the Indian Ocean
(Indian Academy of Sciences, Bangalore, 1988)
Geostrophic velocities are computed across meridians 37 degrees E and 105 degrees E using hydrographic data. The estimated mass transport is represented on a temperature - salinity diagram. The characteristics of the water ...
Watermass structure in the western Indian Ocean: Part 1. Watermasses and their thermohaline indices
(India Meteorological Department, 1986)
The concept of "Indian Ocean Common Watermass" is introduced and its characteristics are defined. The temperature-salinity structures which would result when one, two or more watermasses of different temperature and salinity ...
Variability of wind stress and currents at selected locations over the north Indian Ocean during 1977 and 1979 summer monsoon seasons
(India Meteorological Department, 1988)
Intra-seasonal variability of wind stress, wind stress curl and currents at different locations over the northern Indian Ocean during two contrasting monsoon seasons has been investigated making use of the time series data ...
Watermass structure in the western Indian Ocean - Part 2. The spreading and transformation of the Persian Gulf water
(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 ...
Temperature measurement in the sea
(�Council of Scientific and Industrial Research., 1985)
The importance of measuring sea temperature is explained and the various methods employed for this purpose are reviewed. Instruments used for spot measurement of water temperature at the sea surface and at discrete depths ...