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Numerical model for wind-driven circulation in the Bay of Bengal
(CSIR-NISCAIR, 1986)
Wind-driven circulation in the Bay of Bengal, generated by a southwest wind of constant speed (10 m.sec -1) and direction (225 degrees TN), is presented. A non-linear hydrodynamic model is used for the simulation of ...
Salinity maxima associated with some sub-surface water masses in the upper layers of the Bay of Bengal
(National Institute of Sciences of India, 1968)
The distribution of some sub-surface water masses in the western bay of Bengal during the south-west monsoon period is presented. Based on the salinity maxima and sigma t values the existence of waters of Persian Gulf and ...
On the level of least motion and the circulation in the upper layers of the Bay of Bengal
(National Institute of Sciences of India, 1968)
The paper presents the circulation pattern in the upper 500 metres of the western Bay of Bengal between 9 degrees N and 16 degrees N during the south-west monsoon period, based on the geo-potential anomalies computed from ...