Titlebook: Oceanology of China Seas; Volume 1–2 Zhou Di,Liang Yuan-Bo,Zeng Cheng-Kui (C. K. Tseng) Book 1994 Springer Science+Business Media Dordrecht

Gyrate

Han Wu-ying,Lin Hong-ying,Cai Yan-ya,Rong Rong-gui

得罪

Introductiont 40 years it grew gradually with a series of investigations, such as the Comprehensive Fishery Investigation off Yantai and Weihai (1955), the Investigation in the Bohai Sea and Western Yellow Sea (1957) and the National Oceanographic Investigation (1958-1961). Through these investigations physical

Permanent

都相信我的話

thrombus

Lasting

Estrogen

A Lagrangian model of Circulation in Bohai Seare of interest. The problem of winter circulation in the Bohai Sea is referable to the physics of sea-ice and will be not discussed in this chapter. Preliminary researches suggested that the summer circulation pattern in the Bohai Sea can be grossly characterized by a big counterclockwise gyre (Guan

Dissonance

Three-Dimensional Numerical Modeling of the Water Circulation in South China Seaproach because the acquisition of sufficient field data is very difficult, especially for its deep part, and the topographical complexity hampers the success of analytic solutions even for the simplest models. A basic flow patterns for the upper layer has emerged by 2-D modeling (Guo ., 1983; Wang,

Patrimony

Tides and Tidal Currents in East China Sea, Huanghai Sea and Bohai Sea of two components. The maps of this kind are convenient for tidal current prediction but lack physical meaning. Furthermore, the values are dependent on the choice of the orientation of the coordinate axes. In this chapter we will use the current ellipse parameters to show the characters of the cur

abreast