156-165Distribution of water characteristics and circulation were studied on 260, 160, 140, 120 and 80 cl/t surfaces using isanosteric analysis and geostrophic computation. The circulation pattern consisted of several eddies and meanders. The most prominent anticyclonic eddy was located around 24° N and 64° E. Deepest mixed layer occurred in this region. Appreciably deep vertical extension of the eddies was a notable feature. The eddy circulation is proposed to be due to the influence of uneven bottom topography. Persian Gulf water appeared to flow into the Arabian Sea through the northern part of the Gulf of Oman. Distribution of properties was marked by several pockets of high and low values
Hydrographic and ADCP data were collected in the coastal waters of Oman during the 1987 summer monso...
International audienceA shallow-water model, coupled with a three dimensional, hydrostatic ocean mod...
In this study, we characterize hydrodynamics induced by winds (winter Shamals), tides and baroclinic...
The dynamics and thermodynamics of the surface layer of the Arabian Sea, north of about 10N, are dom...
At intermediate depths of the Arabian Sea, the circulation and characteristics of water are more inf...
Persian Gulf, as an important biological aquatic basin in Middle East, joints via Hormuz Strait to O...
The Persian Gulf produces high-salinity water (Persian Gulf Water, PGW hereafter), which flows into ...
The circulation in the Gulf of Aden is inferred from three different data sets: historical ship dri...
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...
Trajectories and hydrological data from two Argo floats indicate that warm and salty water at 200–30...
International audienceThe Arabian Sea and Sea of Oman circulation and water masses, subject to monso...
This paper provides a detailed hydrographic climatology for the shallow northwestern Arabian Sea pri...
It is the research goal to understand and quantify the physical processes that determine the air-sea...
Hydrographic and ADCP data were collected in the coastal waters of Oman during the 1987 summer monso...
International audienceA shallow-water model, coupled with a three dimensional, hydrostatic ocean mod...
In this study, we characterize hydrodynamics induced by winds (winter Shamals), tides and baroclinic...
The dynamics and thermodynamics of the surface layer of the Arabian Sea, north of about 10N, are dom...
At intermediate depths of the Arabian Sea, the circulation and characteristics of water are more inf...
Persian Gulf, as an important biological aquatic basin in Middle East, joints via Hormuz Strait to O...
The Persian Gulf produces high-salinity water (Persian Gulf Water, PGW hereafter), which flows into ...
The circulation in the Gulf of Aden is inferred from three different data sets: historical ship dri...
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...
Trajectories and hydrological data from two Argo floats indicate that warm and salty water at 200–30...
International audienceThe Arabian Sea and Sea of Oman circulation and water masses, subject to monso...
This paper provides a detailed hydrographic climatology for the shallow northwestern Arabian Sea pri...
It is the research goal to understand and quantify the physical processes that determine the air-sea...
Hydrographic and ADCP data were collected in the coastal waters of Oman during the 1987 summer monso...
International audienceA shallow-water model, coupled with a three dimensional, hydrostatic ocean mod...
In this study, we characterize hydrodynamics induced by winds (winter Shamals), tides and baroclinic...
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