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.
在诸强迫项中,稳定性凝结加热对这一时段梅雨锋暴雨的贡献最大,而对流凝结加热的作用很小。
The stable condensation heating is the most important factor to the maintenance of the storm rainfall during this period.
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