MODELING SEDIMENT TRANSPORT IN THE YELLOW RIVER MOUTH
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Yellow River is famous for its high sediment concentration, which carries a huge amount of sediment into Bohai Sea during the flood season. In the mouth of Yellow River, the suspended sediment concentration (here after: SSC) are relatively high and the average depth is generally shallow. Recent studies indicated that in the shallow and micro-tide area, wave usually is a primary mechanism for bottom sediment resuspension. Most numerical studies of sediment transport in the Yellow River mouth didn't include the wave effects. To analyze the sediment transport in the Yellow River mouth with wave effect, a Coastal Sediment Transport Modeling System (CSTMS) was applied in this study.
2020 ◽
Vol 236
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pp. 106639
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2010 ◽
Vol 30
(1)
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pp. 17-24
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2012 ◽
Vol 212-213
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pp. 351-357
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Response of salinity distribution around the Yellow River mouth to abrupt changes in river discharge
2011 ◽
Vol 31
(6)
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pp. 685-694
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2008 ◽
Vol 28
(14)
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pp. 1782-1790
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2001 ◽
Vol 21
(6-7)
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pp. 607-625
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