【摘 要】
：
Three- dimension (3-D) wind-driven currents in the Bohai Sea in both winter and summer are calculated by using a 3- D barotropic steady model, and the results
【机 构】
：
Institute of Oceanology, Academia Sinica, Qingdao 266071rrrrrrrrn,Ocean University of Qingd
【出 处】
：
Chinese Journal of Oceanology and Limnology
论文部分内容阅读
Three- dimension (3-D) wind-driven currents in the Bohai Sea in both winter and summer are calculated by using a 3- D barotropic steady model, and the results are consistent with observed flow char -acteristics. Based on the results, 3- D characteristics of flow, currents at different depths, compensated flow in the lower layer , long and narrow alongshore current, the area of upwelling and downwelling, main circulation in vertical profile, and the current in Bohai Strait are discussed.
Three-dimension (3-D) wind-driven currents in the Bohai Sea in both winter and summer are using by a 3- D barotropic steady model, and the results are consistent with observed flow char-acteristics. Based on the results, 3- D characteristics of flow, currents at different depths, compensated flow in the lower layer, long and narrow alongshore current, the area of upwelling and downwelling, main circulation in vertical profile, and the current in Bohai Strait are discussed.
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