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Seasonal variation of circulations in the East China Sea and the Yellow Sea

机译:东海和黄海环流的季节性变化

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Seasonal variation of the water circulations in the East China Sea and the Yellow Sea is investigated with use of a robust diagnostic numerical model. Water circulations in four season are calculated diagnostically from the observed water temperature and salinity data from JODC (Japan Oceanographic Data Center) and wind data from COADS (Comprehensive Ocean-Atmosphere Data Set). Counter-clockwise circulations are developed at the upper and middle layers and a clockwise one at the lower layer in the central part of he Yellow Sea in summer. On the other hand, a clockwise circualtion is developed from the surface to the bottom in the Yellow Sea and a counter-clockwise one in, the northern part of the East China Sea in winter.
机译:利用稳健的诊断数值模型研究了东中国海和黄海中水循环的季节性变化。根据从JODC(日本海洋学数据中心)观测到的水温和盐度数据以及来自COADS(综合海洋大气数据集)的风向数据,可诊断地计算出四个季节的水循环。夏季,黄海中部的上层和中层形成逆时针环流,下层则形成顺时针环流。另一方面,在冬季,从表层到底部,顺时针旋转是发展的,而在东海北部,则是逆时针旋转的。

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