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Analysis of the tide on the Hooghly River
Calibration and alteration of a model computing the vertical distribution of the suspended sediment under non-permanent flow conditions
The Hooghly river is situated in West Bengal, a Northeastem state of India. The capital of West Bengal is Calcutta. (See figure 1). The discharge from all the eastem and western tributaries, and from the direct head from the Ganga, flows into the Bay of Bengal through the Hooghly
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