mei yu period 梅汛期
The typical circulation and the related strong precipitation during the Meiyu period over the Yangtze River basin did not appeared,however,the westerlies troughs and landing typhoons brought several rainfall processes to the Yangtze-Huaihe River basin.
江淮梅雨期典型梅雨形势没有建立,为空梅年,但西风槽和登陆台风带来了几次降雨过程。
参考来源 - 2009年夏季异常天气及其环流分析·2,447,543篇论文数据，部分数据来源于NoteExpress
This paper analysed the climate characteristics of the last heavy rain of Mei-yu Period in the NorthZhejiang province from 1961 to 1995.
本文对1961-1995年浙北地区梅汛期末次暴雨的气候特征进行了分析。
Besides, the evolutions of the polar vortex, the trough over Bast Asia and the subtropical high prior to Mei-Yu period are also related to the precipitation during Mei-Yu period.
在前期环流演变中发现极涡、东亚槽、副高等对梅雨的丰枯亦有较好的预兆反映。
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.
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。
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