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The Eddy Northwest of Luzon Island in South China Sea

机译:南海的吕宋岛埃迪西北部

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The Kuroshio intrusion into the SCS through the Luzon Strait is an important process. Because of the intrusion, an eddy is located northwest of Luzon Island. Many papers reported the eddy. However, the eddy was claimed to be either cyclonic or anticyclonic. Based on the P-Vector inverse method, the circulation field is calculated from the GDEM data, and the eddy is identified as cyclonic in the upper layer and as anticyclonic in the lower layer. The results suggest that the anticyclonic eddy originates from Kuroshio intrusion, and the cyclonic eddy is due to the South China Sea Warm Current.
机译:通过吕宋海峡进入SCS的Kuroshio侵入是一个重要的过程。由于入侵,艾迪位于吕宋岛西北部。许多论文报告了埃迪。然而,涡旋被要求是旋风或反气旋。基于P载体逆方法,从GDEM数据计算循环场,并且涡涡体在上层中识别为循环,并且在下层中作为反气旋。结果表明,防寒芯涡流来自于金刚石的侵入,潮流涡流是由于南海暖流。

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