1) Meiyu amount of 2 districts in mid-south Jiangsu
苏南和江淮两区梅雨
3) Meiyu
江淮梅雨
1.
Seasonal variability regarding the nature of precipitation and the activity of cumulus convection during the 1991 Meiyu season of Changjiang Huaihe River Basin (Jianghuai) has been investigated by calculating apparent heat source / apparent moisture sink and analyzing TBB data.
从计算大尺度热源和分析ＴＢＢ资料两个方面，阐述了１９９１年江淮梅雨期间降水性质与对流活动的季节性演变特征。
2.
Based on the precipitation during Meiyu at 37 stations in the Changjiang-Huaihe rivers valley and the mean daily reanalysis geopotential height,wind field,humidity field and surface pressure field data(Grid 2.
5°,采用模糊聚类、合成分析等方法,详细讨论了江淮梅雨丰、枯梅年垂直积分的整层纬向、经向和水汽通量输送差异特征。
4) Jiangsu plum rain
江苏梅雨
1.
Through analyzing the change of south Asia high character index and upper air trough,the impact of South Asia High on Jiangsu plum rain and main precipitation area are discussed.
通过2002～2005年南亚高压特征指数、高空槽变化过程分析,讨论了南压高压对江苏梅雨期和主要降水落区的影响。
6) the excessive rain during Mei-yu rain in Yangtze and Huaihe rivers
江淮梅雨期暴雨
补充资料：南雁荡梅雨瀑
梅雨瀑又称雾瀑云潭，在杜鹃林西边。与杜鹃林一样，在宋代就已知名。此瀑集施岭之水，瀑高30米，宽2～3米。瀑底有梅雨潭。瀑潭三面环山，朝东，每当清晨七时许，朝阳透进山谷，潭角便出现五彩虹霓。梅雨潭右边陡坡上有倒插花岩。“植物本乎地、胡为花倒开？云根分种异，假手自大栽。”明代陈应人曾作诗咏它。上游施岩，传为唐代诗人施肩吾炼丹处。从梅雨瀑下山，过（石丁）砸，到南端桥边转折处，可见金鸡回头峰。但只能在傍晚夜色苍茫时才能窥见她的倩影。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条