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- W2359138564 abstract "A series of numerical experiments were conducted using Princeton Ocean Model (POM) to investigate the behavior and mechanism of the expansion of the Changjiang River diluted water on the shelf of the East China Sea The results show that the bottom topography with variable depths is an essential prerequisite in determining the northeastward expansion of the Changjiang River diluted water in summer The turning of the outflow of the Changjiang River in summer is due to the combined effects of the upwelling favorable wind stress,baroclinicity and bottom topography,whereas the interaction between the wind stress and topography is the main cause On the contrary,in the case of flat bottom,neither the upwelling favorable wind nor the buoyancy forcing induced by the outflow freshwater can make the diluted water turn northeastward Further,without wind forcing,the inflow freshwater induces an anticyclonic eddy near the estuary and a southward coastal current; the former is due to the buoyancy forcing ,while the latter is produced by the mass input from the Changjiang River In the case of flat bottom,the anticyclonic eddy is located in the east of the river mouth When the bottom with variable depths is considered,the anticyclonic eddy is stretched northward,and part of the discharged water flows northward The inflow freshwater can produce a closed vertical circulation cell in the estuary: the freshwater flows seaward in the upper layer and the downwelling occurs around 30-45km away from the coastline; the saline water returns in the lower layer,with the occurrence of upwelling when it meets the seaward inflow around 10 km away from the coastline" @default.
- W2359138564 created "2016-06-24" @default.
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- W2359138564 date "2003-01-01" @default.
- W2359138564 modified "2023-09-28" @default.
- W2359138564 title "NUMERICAL STUDY ON THE MECHANISM OF THE EXPANSION OF THE CHANGJIANG RIVER DILUTED WATER IN SUMMER" @default.
- W2359138564 hasPublicationYear "2003" @default.
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