Zhu Shouxian, Shi Fengyan, Zhu Jianrong, Ding Pingxing. Numerical study on residual current and its impact on mass transport in the Hangzhou Bay and the Changjiang Estuary Ⅰ.A3-D joint model of the Hangzhou Bay and the Changjiang Estuary[J]. Acta Oceanologica Sinica, 2001, (1): 1-13.
Citation:
Zhu Shouxian, Shi Fengyan, Zhu Jianrong, Ding Pingxing. Numerical study on residual current and its impact on mass transport in the Hangzhou Bay and the Changjiang Estuary Ⅰ.A3-D joint model of the Hangzhou Bay and the Changjiang Estuary[J]. Acta Oceanologica Sinica, 2001, (1): 1-13.
Zhu Shouxian, Shi Fengyan, Zhu Jianrong, Ding Pingxing. Numerical study on residual current and its impact on mass transport in the Hangzhou Bay and the Changjiang Estuary Ⅰ.A3-D joint model of the Hangzhou Bay and the Changjiang Estuary[J]. Acta Oceanologica Sinica, 2001, (1): 1-13.
Citation:
Zhu Shouxian, Shi Fengyan, Zhu Jianrong, Ding Pingxing. Numerical study on residual current and its impact on mass transport in the Hangzhou Bay and the Changjiang Estuary Ⅰ.A3-D joint model of the Hangzhou Bay and the Changjiang Estuary[J]. Acta Oceanologica Sinica, 2001, (1): 1-13.
Numerical study on residual current and its impact on mass transport in the Hangzhou Bay and the Changjiang Estuary Ⅰ.A3-D joint model of the Hangzhou Bay and the Changjiang Estuary
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
A 3-D numerical model is set up in a large domain covering the Hang zhou Bay and the Changjiang Estuary based on the ECOM model in orthogonal curvilinear coordinates.The numerical schemes for baroclinic pressure gradient (BPG) terms and convective terms are improved in the paper according to the characteristics of velocity field and mass transport in the area.The model is validated by the simulations of residual current and salinity transport in the Hangzhou Bay and the Changjiang Estuary.
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