梅雨,meiyu
1)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
英文短句/例句

1.Things easily get mildewed in the rainy season.梅雨季节东西容易发霉。
2.At the foot of the pavilion is the deep Plum Rain Pool.亭下深深的便是梅雨潭。
3.CHARACTERS OF THE WATER VAPOR TRANSFER IN THE CHANGJIANG-HUAIHE RIVERS VALLEY江淮梅雨丰、枯梅年水汽输送差异特征
4.ON THE RELATIONSHIP BETWEEN MEIYU HEAVY RAINFALL OVER THE JIANG HUAI BASIN IN 1991 AND ASIAN MONSOON1991年江淮梅雨暴雨与亚洲季风的关系
5.The Structure and Character of Mei yu Front Storm over the Middle and Lower of Yangtze River长江中下游梅雨锋暴雨的结构和特征
6.The Diagnoses and Simulation of Rainstorms Taken Place in Jianghuai Area in Meiyu Period of 2003;2003年江淮梅雨暴雨的诊断与数值模拟
7.A Case Study on Dynamics of Summer Rainstorm in Meiyu Period in Huangshan Mountain Area黄山地区梅雨期暴雨个例的诊断分析
8.Plum Rain Pool is at the foot of a waterfall, the lowest of the three waterfalls on Xianyan.梅雨潭是一个瀑布潭。 仙岩有三个瀑布,梅雨瀑最低。
9.Meiyu in Middle and Low Reaches of Yangtze River, Its Relationship with General Atomspheric Circulation and Forecast Experiments on Meiyu;长江中下游地区梅雨及其与环流的联系和梅雨预测试验
10.Analysis on Large-Scale Circulation Characteristic of Meiyu Rainstorm and Structure of Meiyu Front in Zhejiang Province during 20082008年浙江梅汛期暴雨的大尺度环流特征及其梅雨锋结构分析
11.Mesoscale Feature and Orographic Sensitivity Test of "07.7" Meiyu Front Rainstorm;“07.7”梅雨锋暴雨中尺度特征及地形敏感性试验
12.Numerical Simulation and Diagnostic Analysis of Meiyu Front Rainstorms in 2005;2005年梅雨锋暴雨的数值模拟及诊断分析
13.Numerical Study of the Evolution Mechanism of Mesoscale System for "05·7" Meiyu Front Rainstorm;“05.7”梅雨锋暴雨中尺度系统发展演变的数值研究
14.The Model Experiment and Analysis of the Meso-Scale Systems in the Course of Meiyu Frontal Rainstorm;梅雨锋暴雨中尺度系统的模式试验和分析
15.Mesoscale System and Numerical Simulation Analysis of Heavy Rain in Hubei Province during Meiyu Season湖北省梅雨期暴雨的中尺度系统及其模拟分析
16.Mesoscale Characteristics Analysis of a Meiyu Front Heavy Rain Process一次梅雨锋暴雨过程的中尺度特征分析
17.Diagnostic Analysis on Maintenance Mechanism of Meiyu Front Rainstorm during 4~5 July 20032003年7月4~5日梅雨锋暴雨维持的诊断分析
18.Orographic Sensitivity Experiments of "07.7" Meiyu Front Rainstorm“07.7”淮河流域梅雨锋暴雨的地形敏感性试验
相关短句/例句

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)precipitation type during the Mei-yu period梅雨雨型
5)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。
6)meiyu rain-band梅雨雨带
延伸阅读

梅雨梅雨春末夏初(5月底~7月初)中国长江、淮河流域和日本南部的连阴雨天气。由极地冷气团和副热带暖气团在这一带交绥所致。因空气潮湿,衣物容易发霉,又时值梅子黄熟,故称梅雨,又称霉雨和黄梅雨。梅雨时日又称黄梅天、黄梅季。由于各年冷暖气流的强弱和进退迟早不同,梅雨期出现的早晚、长短和雨量的多寡变化较大。梅雨适时适量有利于农作物生长;若雨期过长或过短,雨量过多或过少,则可引起旱涝灾害。