The role of wind on the detachment of low salinity water in the Changjiang Estuary in summer
Two detachment processes of low salinity water (LSW) in the Changjiang Estuary in July 2006,and the role of wind on detaching the LSW in particular,are explored with a three-dimensional numerical model.Results show that wind is the most important dynamic factor in the two detachment processes of the LSW.Wind mixing,wind-driven northward current and wind-induced upwelling are three driving forces on detaching the LSW,which increase the salinity in the upper layer in the detachment region along the 30 m isobaths and separate the offshore LSW from the near-shore main body of LSW.The diagnostic analysis further indicates that the increase of salinity in the detachment region is mainly due to northward current which transports high salinity water from the south.
Changjiang diluted water Low salinity water Detachment process
Ji-Liang Xuan Daji Huang Feng Zhou Xiao-Hua Zhu Xiaopeng Fan
State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, State Oceanic Administration, Hangzhou, China, 310012
国际会议
The 17th Pacific -Asian Marginal Seas Meeting(第十七届太平洋与亚洲边缘海国际会议)
杭州
英文
133-138
2013-04-23(万方平台首次上网日期,不代表论文的发表时间)