1)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。
英文短句/例句
1.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
2.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
3.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
4.Mesoscale Predictability Study on a Mei-Yu Frontal Heavy Rainfall over Changjiang-Huaihe Basin一次江淮梅雨锋暴雨的数值模拟可预报性研究
5.Analysis of the Meiyu Gernal Circulation Characteristics and Impact Factors over the Changjiang-Huaihe Valley;江淮梅雨异常大气环流特征及其影响因子分析
6.Possible Reasons for Northward Shift of Meiyu Belt in Yangtze-Huaihe River Region During 2000-20052000年以来江淮梅雨带北移的可能成因分析
7.Relationship between Atmospheric Heat Source in Tibetan Plateau and Abnormality of Meiyu in Changjiang-Huaihe River Valley青藏高原大气热源与江淮梅雨异常的关系
8.Diagnostic Analysis and Numerical Simulation of the Mesoscale System during "03.7" Meiyu Frontal Rainstorm Event;“03.7”江淮梅雨锋暴雨中尺度系统的诊断与模拟研究
9.A Numerical Simulation Study of Abnormal Meiyu in Yangtze-Huaihe Region and the Data Assimilation of Soil Moisture on Its Improvement;江淮梅雨异常的数值模拟及土壤湿度资料同化对其模拟的改进
10.Analysis to the Impacts of the Northeast Cold Vortex (NECV) Process on the Rainfall during Meiyu Period over the Yangtze-Huaihe River;东北冷涡过程对江淮梅雨期降水影响机制的分析
11.Evaluation of meiyu prediction in the Yangtze-Huaihe region by coupled Ocean-Atmosphere General Circulation Model(BCC_CM1.0)全球海气耦合模式(BCC_CM1.0)对江淮梅雨降水预报的检验
12.Relationship between Characteristics of Perturbation & Average Water Vapor Transport in Asian-Australian Moonsoon Area and Jianghuai Meiyu Anomaly;亚澳季风区平均场和扰动场水汽输送特征及其与江淮梅雨异常的关系
13.Numerical Simulation and Diagnostic Analysis of Moisture Helicity in a Meiyu Front Heavy Rain in Changjiang-Huaihe Basins in 2004;2004江淮一次梅雨暴雨中水汽螺旋度的数值研究和诊断分析
14.Primary Research &. Analysis on the Dynamical Mechansim of Heavy Rain over Changjiang-Huaihe River Basin during the Meiyu Period;梅雨期江淮暴雨发生发展动力学机制的初步分析研究
15.The Mechamism Analysis and Numerical Simulation Study on the Meiyu Heavy Rainfall on 5～(th) July 2003 in the Changjiang-Huaihe River Basin;2003年7月5日江淮流域梅雨锋暴雨的机制分析及数值模拟
16.Analysis on the Climate Properties of Meiyu Season and Its Anomalies over Changjiang River and the Huaihe River Basins;江淮流域梅雨季节的气候特征及其异常的分析研究
17.Anomalies of Extreme Precipitation during the Meiyu Period of JiangHuai Valleys and Its General Circulation Characteristics;江淮地区梅雨期极端降水异常及其环流特征分析
18.SVD Analysis of the Relationship between Jianghuai Region Meiyu Season Precipitation and the Sea Surface Temperature and Related Numerical Simulation;江淮地区梅雨期降水与海温的SVD分析及相关数值模拟
相关短句/例句
Changjiang-huaihe Meiyu period江淮梅雨期
3)the excessive rain during Mei-yu rain in Yangtze and Huaihe rivers江淮梅雨期暴雨
4)Meiyu in the Yangtze-Huaihe region江淮地区梅雨
5)Meiyu in the Yangtze River-Huaihe River valley江淮流域梅雨
6)Classification of Meiyu precipitation in Yangtze-Huaihe region江淮梅雨分型
延伸阅读
江淮梅雨锋暴雨江淮梅雨锋暴雨rainstorm caused by plum rain front in Jiang-Huai Valleys 1 ianghuai meiyufeng baoyu江淮梅雨锋暴雨(rainstorm eaused byPlum rain front in Jiang·Huai Valleys)每年6、7月间发生在长江中下游和淮河地区的锋面暴雨。这一时期，由于大气环流的季风调整，来自海洋的暖湿气流与北方南下的冷空气在江淮流域持续交绥，形成一条东西向准静止锋，一般称为梅雨锋，造成阴雨连绵和暴雨集中的天气。此时正值江南梅子黄熟时期，故称“梅雨”或‘’黄梅天气”;又因这时高温高湿，衣物容易霉烂，也有“霉雨”之说。在梅雨时期，从江淮流域至日本南部，维持一条稳定持久的雨带。雨带中的暴雨分布不均匀。有一个个暴雨雨团。梅雨锋暴雨的强度一般比台风暴雨要小得多，但由于梅雨锋持续时间长，暴雨面积广，造成的洪涝灾害区一般比台风要大。如1954年江淮流域梅雨期持续约50天。大部分地区出现了暴雨天气和严重的洪涝灾害。同时又与长江上游的洪水遭遇，长江中下游干流洪峰水位创实测历史最高记录，受灾害面积之广，持续时间之长均为历史罕见。梅雨锋暴雨是在特定的大型环流条件下由天气尺度系统和中小尺度天气系统形成的。大型环流条件一般包括:①在亚洲的高纬度地区对流层中部有阻塞高压或稳定的高压脊，大型环流相对稳定少变;②中纬度地区西风环流平直，频繁的短波活动为江淮地区提供冷空气条件;③西太平洋副热带高压有一次明显西伸北跳过程，500百帕副高脊线稳定在北纬200至25’之间，暖湿气流从副高边缘输送到江淮流域。在这种环流条件下，梅雨锋徘徊于江淮流域，并常常伴有西南涡和切变线，在梅雨锋上中尺度天气系统活跃不仅维持了梅雨期连续性降水，而且为暴雨提供了充沛的水气，暖湿不稳定空气层结和强烈的低空辐合。梅雨锋暴雨是不同尺度环流系统相互作用下形成的一种特定地区的特殊天气，大气环流的变异性，导致各年江淮流域梅雨开始期有迟有早，梅雨持续时间有长有短，在一些年份，梅雨锋特别活跃，暴雨频繁，造成洪涝灾害，在另一些年份，梅雨锋不明显，出现“空梅”，形成干早天气，江淮流域梅雨结束后，雨带移至华北地区，江淮流域进入高温少雨天气。(黄忠怒)
