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Circulation Patterns of Summer Monsoon Corresponding to Two Kinds of Indices over the South China Sea

机译:南海夏季风与两种指数对应的环流模式

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The characteristics of circulation corresponding to two kinds of indices of summer monsoon onset over the South China Sea (SCS) have been discussed using the reanalysis data of the National Centers for Environmental Prediction-National Center for Atmospheric Research. It is found that there are two patterns of deep convection that occur at different locationsand influence the summer monsoon onset over the SCS. One is over the Asia continent and the western Pacific corresponding to the southwesterly of summer monsoon prevailing over the northern and central part of the SCS, while the other is near the Philippines that affects the westerly summer monsoon as prevailing over the central and southern part of the SCS. Since these two kinds of convection affecting the summer monsoon onset do not always occur together, thus the summer monsoon onset time is different when determined by various indices.
机译:利用国家环境预测中心—国家大气研究中心的再分析资料,讨论了与南海夏季风爆发的两种指标相对应的环流特征。结果发现,深对流有两种模式发生在不同的位置,并影响南海夏季风的爆发。一个在亚洲大陆和西太平洋上空,对应于南海北部和中部盛行的夏季风的西南方向,另一个在菲律宾附近,影响西风的夏季季风,盛行于南海的中部和南部。 SCS。由于影响夏季风爆发的这两种对流并不总是同时发生,因此当通过各种指标确定时,夏季风爆发时间是不同的。

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