A barotropic numerical model is employed to explain some of the observed features. Reasonable simulation of the circulation in the northeast part of SCS has been found.
使用一个正压数值模式,解释了一些观测到的特征,得到了南海东北部环流合理的模拟。
A barotropic numerical model is employed to explain some of the observed features. Reasonable simulation of the circulation in the northeast part of SCS has been found.
使用一个正压数值模式,解释了一些观测到的特征,得到了南海东北部环流合理的模拟。
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