Numerical experiments on the wind-driven circulation in the Bohai, Huanghai and East China Seas in winter
- 43 Downloads
A new semi-implicit numerical model developed to investigaté the wind-driven circulation (with inflow and outflow) in the Bohai, Huanghai and East China Sea in winter showed that the open boundary conditions and wind forcing are important in controlling general circulation in wintertime; that open boundary conditions (such as Kuroshio, Changjiang River runoff) are primary factors controlling the East China Sea circulation; and that wind driven current is more important in the upper layer in shallow sea area (such as Bohai Sea, North Huanghai Sea, as well as coastal area) in winter. Two numerical experiments are discussed to demonstrate the circulation responding to the changes of the open boundary conditions.
Key wordsBohai Sea Huanghai Sea East China Sea winter circulation numerical experiment
Unable to display preview. Download preview PDF.
- Feng Shizuo, 1987. A three-dimensional weakly nonlinear model of tide-induced Lagrangian residual current and mass-transport, with an application to the Bohai Sea.In: Three-dimensional Model of Marine and Estuarine Dynamics, ed. by J. C. J. Nihoul and B. M. Jamart, Elsevier Science Pub., Com., Amsterdam-Oxford-New York, p. 471–488.Google Scholar
- Feng, S., 1998. On the Circulation in Bohai Sea, Yellow Sea and East China Sea.In: Health of the Yellow Sea, ed. by G. H. Hong et al., KORDI, Korea, p. 43–78.Google Scholar
- Guan Binxian, Mao Hanli, 1982. A note on circulation of the East China Sea.Chin. J. Oceanol. Limnol. 1(1): 5–16.Google Scholar
- Guo Binghuo, Lu Jingming, Lin Kuiet al., 1987. Some features on the circulation in the East China Sea, Essays on the investigation of Kuroshio. Ocean Press, Beijing, p. 32–43.Google Scholar
- Keller, H. B., 1976. Numerical solution of two point boundary value problems. Society of Industrial and Applied Mathematics, J. W. Arrowsmith Ltd., 61p.Google Scholar
- Nakao, Toru, 1977. Oceanic variability in relation to fisheries in the East China Sea and the Yellow Sea.Journal of the Faculty of Marine Science and Technology, Tokai Univ., Spec., Nov:199–362.Google Scholar
- Sun Wenxin, 1992. A numerical method of 3-D shallow sea fluid dynamic-the Current Splitting Method (edited by Feng Shizuo and Sun Wenxin), Science and Technology Press of Henan Province, p. 100–195. (in Chinese)Google Scholar
- Wang Hui, 1995. Baroclinic model of winter circulation in the East China Sea and South Yellow Sea.Acta Oceanologica Sinica 17(2):21–26 (in Chinese)Google Scholar
- Xi Pangeng, Zhang Shuzhen, Feng Shizuo, 1980. A circulation model of the East China Sea (I).J. Ocean. College of Shandong 10(3): 13–25 (in Chinese, with English abstract)Google Scholar
- Yuan Yaochu, Su Jilan, Zhao Jinshen, 1982. A one-layer continental shelf model of the East China Sea.Acta Oceanologica Sinica 4(1):1–10. (in Chinese)Google Scholar
- Zhao Baoren, Fang Guohong, 1991. The estimated flux of main channels in the East China Sea.Acta Oceanogica Sinica 13(2):169–178. (in Chinese)Google Scholar