At intermediate depths of the Arabian Sea, the circulation and characteristics of water are more influenced by the high saline waters from the north and low saline waters from the south of equator. The interaction of these waters which greatly differ in characteristics is less understood compared to that at the upper layers. An understanding of the nature of the intermediate waters is of vital importance not only because of the unusual characteristics of the waters but also due to the influx of the different water masses from the neighbouring Red Sea and Persian Gulf. Hence, in the present investigation, it is proposed to study the water characteristics and current structure of the intermediate waters in the Arabian Sea through the distribu...
271-277In the Arabian Sea surface salinity (S-O) is more than 35 PSU throughout the year, except in ...
The euphotic zone of the northern Arabian Sea ranges from 20 to 60 m with an average depth of about ...
We investigate the variability of the circulation, water masses, heat and salt fluxes in the Arabian...
234-240After the cessation ofthe SW monsoon over Arabian Sea, the North Equatorial Current sets stro...
1-6Circulation pattern in the Arabian Sea is derived from computation of acceleration potential at 2...
Levitus (1982) climatology has been used to identify four extrema, three maxima and one minimum, in ...
156-165Distribution of water characteristics and circulation were studied on 260, 160, 140, 120 and ...
Typescript.Bibliography: leaves 131-133.xi, 133 l charts, graphs, maps, tablesContraction of volume ...
136-140Three water masses in the Arabian Sea have been identified from their physical and chemical c...
The present investigatioh concerns itself with two problems: First it is investigated with the aid o...
This study uses the relationship between conservative chemical parameters and the relationship betwe...
Abstract. As a result of its remarkably high salinity and despite its small volume input, remnants o...
The dynamics and thermodynamics of the surface layer of the Arabian Sea, north of about 10N, are dom...
International audienceIn the Indian Ocean, salty water masses from the Persian Gulf and Red Sea are ...
321-326Spreading of the Persian Gulf Watermass in the intermediate layers and the process of mixing ...
271-277In the Arabian Sea surface salinity (S-O) is more than 35 PSU throughout the year, except in ...
The euphotic zone of the northern Arabian Sea ranges from 20 to 60 m with an average depth of about ...
We investigate the variability of the circulation, water masses, heat and salt fluxes in the Arabian...
234-240After the cessation ofthe SW monsoon over Arabian Sea, the North Equatorial Current sets stro...
1-6Circulation pattern in the Arabian Sea is derived from computation of acceleration potential at 2...
Levitus (1982) climatology has been used to identify four extrema, three maxima and one minimum, in ...
156-165Distribution of water characteristics and circulation were studied on 260, 160, 140, 120 and ...
Typescript.Bibliography: leaves 131-133.xi, 133 l charts, graphs, maps, tablesContraction of volume ...
136-140Three water masses in the Arabian Sea have been identified from their physical and chemical c...
The present investigatioh concerns itself with two problems: First it is investigated with the aid o...
This study uses the relationship between conservative chemical parameters and the relationship betwe...
Abstract. As a result of its remarkably high salinity and despite its small volume input, remnants o...
The dynamics and thermodynamics of the surface layer of the Arabian Sea, north of about 10N, are dom...
International audienceIn the Indian Ocean, salty water masses from the Persian Gulf and Red Sea are ...
321-326Spreading of the Persian Gulf Watermass in the intermediate layers and the process of mixing ...
271-277In the Arabian Sea surface salinity (S-O) is more than 35 PSU throughout the year, except in ...
The euphotic zone of the northern Arabian Sea ranges from 20 to 60 m with an average depth of about ...
We investigate the variability of the circulation, water masses, heat and salt fluxes in the Arabian...