1)Meiyu front梅雨锋
1.The Initial Error Analysis of Mesoscale Low on Meiyu Front Based on the Pseudo-inverse Perturbation;基于假反扰动的江淮梅雨锋低涡初始误差分析
2.Simulation study of three-dimensional airflow structure of mesovortexes along Meiyu front;梅雨锋低涡系统三维流场结构的分析
3.Relationship between the evolvement of Meiyu front and the vortex along it.;梅雨锋演变与低涡发展的联系
英文短句/例句
1.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
2.The Similarities and Differences Between the Quasi-stationary Front in the Winter of 2008 and the Meiyu Front in the Summer of 19982008年冬季准静止锋与1998年夏季梅雨锋的异同
3.STRUCTURE AND FORMATION OF MEI-YU FRONT IN 19981998梅雨锋的结构特征及形成与维持
4.THE MESOSCALE ANALYSIS OF THE MEI-YU FRONT CLOUD SYSTEM IN 19911991年梅雨锋云系的中尺度分析
5.Study on Mesoscale Structures of Cloud Physical Processes in Mei-Yu Front System in June 1999;“99.6”梅雨锋降水云物理过程研究
6.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
7.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
8.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
9.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
10.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
11.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
12.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
13.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
14.Structure of Meiyu Front and Its Sensitivity Experiment of Relationship between Front and Vortex Disturbance一次梅雨锋结构及锋区强度对锋面结构影响的数值模拟
15.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
16.Analysis of Persistent Heavy Rainfall in the font of Upper Trough Associated the Meiyu Front-the Case over the Sichuan Basin during July 1981梅雨锋西端高空低压槽前持续性暴雨分析——1981年7月四川大暴雨
17.Study on cloud micro-physical processes and precipitation formative mechanisms of a mesoscale convective system in Meiyu front in June 2004一次梅雨锋上MCS云微物理过程及降水形成机制
18.Relationship Between the Upper Flow Divergent over the Northern Flank of Southern Asiatic High and the Development of Heavy Rain over Mei-Front南亚高压北缘的高空气流发散与梅雨锋暴雨发展的关系
相关短句/例句
Mei-yu front梅雨锋
1.The heavy rainfall event of June 27, 1981 in the Mei-Yu front as a case is slmulated byusing the mesoscale model MM5.本文利用中尺度数值模式MM5，选取1981年6月27日梅雨锋暴雨个例进行数值模拟，分析了梅雨锋上的中β尺度雨团和中β尺度系统的空间结构特征。
3)Meiyu front system梅雨锋系
4)Meiyu forntal zone梅雨锋区
5)Meiyu front rainstorm梅雨锋暴雨
1.Numerical simulation tests of three representative Meiyu front rainstorm processes of the Huai-he flood reason in July 2003 were conducted with WRF(weather research and forecasting) model for the intention of investigating the applicability of WRF model to research and forecast our country s rainstorm.为了分析天气研究及预报WRF(weather research and forecasting)模式对我国天气现象的适用性,利用WRF模式对2003年淮河汛期的3次梅雨锋暴雨过程进行了一组数值模拟试验,对3次天气过程模拟试验采用相同的参数设置,模拟区域根据实况降水落区作了相应设置。
2.6") Meiyu front rainstorm are analyzed using the observed data and the high-resolution output from the numerical simulation.6”)的一次梅雨锋暴雨β中尺度系统结构和演化及其发展机理进行了研究,分析发现:(1)此次暴雨过程发生在500 hPa东亚大槽不断加深发展的阶段,也是中纬度大气长波调整的时期。
3.The purpose is to investigate the influence of various moist physical schemes on the forecasted precipitation of Meiyu front rainstorm.利用 PSU/NCAR的 MM5对 1 999年 6月下旬发生在江淮流域的梅雨锋暴雨进行数值模拟试验 ,研究 MM5中不同湿物理过程对 MM5模拟梅雨锋暴雨的影响。
6)Meiyu front heavy rain梅雨锋暴雨
1.Through the diagnosis of a Meiyu front heavy rain process occurring from 1 to 3 June, 2000, this paper has studied the affection on the rainstorm caused by the ageostrophic wind, the unbalanced flow, low level jet (LLJ), and the generation and propagation of gravity wave after the abrupt change in large-scale circulations.文中以 2 0 0 0年 6月 1～ 3日的一次梅雨锋暴雨过程为例 ,通过数值模拟 ,得到了降雨区和强度都与实况基本吻合的结果。
2.Using the wet Q-vector and combining with the intense data output of the modified MM4(MMM4) model simulation,a typical Meiyu front heavy rain process occurred during 5-6th July 1991 in the Changjiang-Huaihe Basin is diagnosed carefully in this paper.利用湿 Q矢量 ,结合改进的 MM4 ( MMM4 )模式模拟输出的加密资料 ,细致地诊断分析了 1 991 - 0 7- 0 5T2 0— 0 6 T2 0一次典型的江淮梅雨锋暴雨过程。
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)
