与副热带锋区上急流相关的平流非线性作用在水热收支与涡度平衡中占优势。
Nonline advection which is connected with jet of subtropical frontal zone occupies a main place in heat and moisture budgets and vorticity balance.
研究表明，出现强降水时的梅雨锋结构已经变性或者说它是介于温带锋面结构和ITCZ结构之间的副热带锋系结构。
IT is pointed out that the nature of the Mei-Yu front's structures has changed into the sub-tropical style, something between extratropical fronts and ITCZ during the torrential rain period.
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