1) Meiyu variations
梅雨演变
2) Mei-Yu
梅雨
1.
Mei-yu,Arctic Oscillation and stratospheric circulation anomalies;
梅雨与北极涛动及平流层环流异常的关联
2.
The Piecewise Potential Vorticity Inversion s Application in the Interaction between Mei-yu Precipitation and the Western Subtropical High;
分片位涡反演在梅雨锋降水和西太副高相互作用研究中的应用
3.
In this paper,the total rainfalls data of 40 years in Mei-Yu season of fivestations (i.
本文根据里下河地区建湖、兴化、盐城、宝应和阜宁共5个代表站，对1954-1993年共40年的梅雨期降水量和西太平洋副高脊线、588位势什米的西脊点等资料进行分析，发现里下河地区洪涝灾害与梅雨期开始时间早、持续时间长、暴雨频发和雨带稳定在里下河地区有关，而后者又与副热带高压活动特点以及西风带环流特征有密切的关系。
3) Plum rains
梅雨
1.
Contrastive analysis of plum rains floods in typical years in Jiangsu Province;
江苏省典型年梅雨洪涝灾害对比分析
4) meiyu
梅雨
1.
Impacts of longitude location changes of East Asian westerly jet core on the precipitation distribution during meiyu period in middle-lower reaches of Yangtze River valley;
高空西风急流东西向形态变化对梅雨期降水空间分布的影响
2.
Location of Rainbelt of Meiyu During Second Half of 19th Century to Early 20th Century;
19世纪后半叶至20世纪初叶梅雨带位置的初步推断
3.
Temporal Evolution and Spatial Distribution Characteristics of Meiyu in Changjiang-Huaihe River Valley;
江淮梅雨的时空变化特征
5) precipitation type during the Mei-yu period
梅雨雨型
6) Meiyu rainstorm
梅雨暴雨
1.
Meiyu rainstorms occurred in the Changjiang-Huaihe River valley in 2003 are classified into four categories according to the convective stability and precipitation property at the center of rainstorm,and the ralationships of moist potential vorticity with inertial,symmetry,and convective instabilities are analyzed.
统计了2003年发生在江淮地区的梅雨暴雨,根据暴雨中心对流稳定度及降雨性质将暴雨分为4种类型。
2.
Diagnostic analyses are carried out for the Meiyu rainstorm in the Meiyu period from 0000UTC 20th July to 1200UTC 1st August in 1998 and the MM5V3 meso-scale model is used to simulate the Meiyu rainstorm.
对1998年7月20日00时—8月1日12时这段梅雨暴雨过程进行诊断分析,并利用MM5V3中尺度模式作梅雨暴雨的数值试验,结果表明:(1)本次梅雨暴雨分为3大段过程,非线性亚临界对称不稳定可能是3段梅雨暴雨形成的重要机制;(2)扰动风场增长与降水增长关系密切,扰动风场的增长会超前于降水的增长,非线性亚临界对称不稳定的增强可能使降水增强;(3)非线性亚临界对称不稳定主要发生在高层200hPa,中层500hPa也有发生。
补充资料：大洋环流的演变
见古海洋学。
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