Zhu Shouxian, Dang Pingxing, Shi Fengyan, Zhu Jianrong. Numerical study on residual current and its impact on mass transport in the Hangzhou Bay and the Changjiang Estuary Ⅱ. Residual current and its impact on mass transport in winter[J]. Acta Oceanologica Sinica, 2001, (2): 153-169.
Citation:
Zhu Shouxian, Dang Pingxing, Shi Fengyan, Zhu Jianrong. Numerical study on residual current and its impact on mass transport in the Hangzhou Bay and the Changjiang Estuary Ⅱ. Residual current and its impact on mass transport in winter[J]. Acta Oceanologica Sinica, 2001, (2): 153-169.
Zhu Shouxian, Dang Pingxing, Shi Fengyan, Zhu Jianrong. Numerical study on residual current and its impact on mass transport in the Hangzhou Bay and the Changjiang Estuary Ⅱ. Residual current and its impact on mass transport in winter[J]. Acta Oceanologica Sinica, 2001, (2): 153-169.
Citation:
Zhu Shouxian, Dang Pingxing, Shi Fengyan, Zhu Jianrong. Numerical study on residual current and its impact on mass transport in the Hangzhou Bay and the Changjiang Estuary Ⅱ. Residual current and its impact on mass transport in winter[J]. Acta Oceanologica Sinica, 2001, (2): 153-169.
Numerical study on residual current and its impact on mass transport in the Hangzhou Bay and the Changjiang Estuary Ⅱ. Residual current and its impact on mass transport in winter
State Key Laboratory of Estuarine and Coastal research, East China Normal University, Shanghai 200062, China;Meteorology Institute of the PLA Science and Engineering University, Nanjing 211101, China
2.
State Key Laboratory of Estuarine and Coastal research, East China Normal University, Shanghai 200062, China
Some observational characteristics of residual current and mass transport in the Hangzhou Bay and the Changjiang Estuary in winter are analyzed.The residual current and its impact on mass transport are simulated with a 3-D joint model for the Hangzhou Bay and the Changjiang Estuary,in which the impacts of river flux,wind,baroclinic pressure gradient (BPG),background current in the East China Sea and tide (including M2,S2,K1 and O1) are taken into account.Based on these studies,further simulations are made to analyze the dynamical mechanisms of the observational characteristics.
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