Simulations of Lagrangian Residual Current in Changjiang Estuary, Hangzhou Bay and Their Adjacent Area
The Lagrangian circulation in Changjiang Estuary, Hangzhou Bay and their adjacent sea area is simulated, with the riverine discharge, East China Sea Current, wind, the major tidal components, and the density gradient taken into account. The modeled outputs show that surface circulation pattern is similar to depth-averaged one both in summer and in winter. The Taiwan Warm Current is stronger due to the relatively large horizontal density gradient in summer. Dominated by tidalinduced current and wind-driven current, the pattern of circulation in Hangzhou Bay is against transporting material outward in winter, especially in the bay head, while it is in contrast in summer.
Lagrangian circulation Changjiang Estuary Hangzhou Bay The Taiwan Warm Current
Tao ZOU Zhe LIU Hui-wang GAO Wen-xin SUN
Key Laboratory of Marine Environment and Ecology (Ocean University of China) Ministry of Education o Key Laboratory of Physical Oceanography (Ocean University of China) Ministry of Education of China (
国际会议
北京
英文
1-3
2009-06-11(万方平台首次上网日期,不代表论文的发表时间)