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Extra info for Advances in Geosciences: Volume 10: Atmospheric Science (As)
The positive EASM’s index anomalies cover the mid-lower of Yangtze Valley while negative anomalies cover South China and North China. Westerly anomalies appear in Yangtze River and northerly ﬂows control South China and North China (Fig. 7(c)).
The weak descending motion in front of the monsoon convection helps to preserve the converged moisture near the surface. The air temperature proﬁle observed from AIRS satellite show that a relatively warm center lies in front of the rainfall maximum while a cold one overlapping the rainfall maximum. Therefore, the monsoon rainfall maximum is overlapped and followed by a dry-cold ABL and preceded by a warm–wet one. This provides a favorable condition for the northward migration of the convection from southern to northern SCS.
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