Based on a 3-D dynamic numerical model of primitive equation, the general circulation in the East China Sea and the Yellow Sea was studied with a 0.25 ° ×0.25 ° horizontal grid and a realistic bottom to...Based on a 3-D dynamic numerical model of primitive equation, the general circulation in the East China Sea and the Yellow Sea was studied with a 0.25 ° ×0.25 ° horizontal grid and a realistic bottom topography. The tidal current and Kuroshio (Japan current) were considered. The main results of the general circulation in the East China Sea and the Yellow Sea were obtained. The numerical results were compared with the observed results. The compared results show that 3-D dynamic numerical model is efficient to predict general circulation in the East China Sea and the Yellow Sea.展开更多
文摘Based on a 3-D dynamic numerical model of primitive equation, the general circulation in the East China Sea and the Yellow Sea was studied with a 0.25 ° ×0.25 ° horizontal grid and a realistic bottom topography. The tidal current and Kuroshio (Japan current) were considered. The main results of the general circulation in the East China Sea and the Yellow Sea were obtained. The numerical results were compared with the observed results. The compared results show that 3-D dynamic numerical model is efficient to predict general circulation in the East China Sea and the Yellow Sea.
