1)persistent heavy rain in South China华南致洪暴雨
英文短句/例句
1.Diagnosis and Predictability of the Persistent Heavy Rainfall Event in South China in June 2005;2005年6月华南致洪暴雨的成因分析及可预报性研究
2.Simulation Sensitivity to Initial and Boundary Condition Uncertainties of a Persistent Heavy Rainfall Event in South China with AREM Model初边界条件不确定性对AREM模拟一次华南致洪暴雨的影响
3.The Research on the Activity of Southwest Vortex and Flood-producing Rainstorm Influencing South of China;影响华南的西南低涡及其致洪暴雨的机理研究
4.The torrential rains that triggered the flooding were expected to continue over the next couple of days, Xinhua said.据新华社消息，由暴雨导致的洪水在未来几天仍将持续。
5.Analysis of Multi-scale System and Numerical Modeling of a June 2005 Torrential Rain over South China;0506华南致灾暴雨的多尺度分析和数值模拟
6.There was a heavy rain, causing floods in the area.天降暴雨，导致那个地区洪水泛滥。
7.The Key Technique Research of Forecasting and Early-warning System on Flood-induced Heavy Rain;致洪暴雨预报预警系统关键技术研究
8.Analysis of Flood-causing Rainstorm over the Wujiang River Basin in June 20082008年6月武江流域致洪暴雨过程分析
9.A CASE STUDY ON A HEAVY RAINFALL EVENT HAPPENED IN LINCANG CITY ON THE 20TH OF JULY 2007临沧市“2007.7.20”致洪暴雨成因分析
10.Thirty-five people are dead and 11 are missing as rainstorms continue to lash southwest China"s Chongqing municipality, according to the municipal flood control office.中国西南部直辖市重庆市市政洪水控制办公室声称，持续暴雨已导致35人死亡，11人失踪。
11.The storms have caused mountain torrents and mud-rock flows, resulting in transportation blocks.暴风雨导致了山洪和泥石流，造成交通堵塞。
12.The wind will bring heavy rain to some places and then brings about floods.强风将导致一些地方下暴雨，而后就是洪灾了。
13.Research and Development of Forecasting and Early-warning Information Issuance System on Flood-induced Heavy Rain;致洪暴雨预测预警信息发布系统的研究与开发
14.Study on Hydro-meteorological Forecasting Model of Flood Caused by Torrential Rain in Plain River Network Region平原河网区暴雨致洪的水文气象预报模型研究
15.The Mountainous Area Sends the Rainstorm Early Warning Signal Issue Operation Flow the Ponder山区致洪暴雨预警信号发布业务流程的思考
16.Meso-scale characteristics analysis of a flash flood-inducing rainstorm over Huaihe River Basin淮河流域一次致洪大暴雨的中尺度特征分析
17.Analysis of Flooding Rainstorm Caused by MCC Over North Jiangsu Province江苏北部一次由MCC引发的致洪暴雨综合分析
18.Analysis and Countermeasure of Flood Calamity Cause of Jinan City"7.18"Catastrophic Rainstorm济南市“7.18”特大暴雨洪水灾害成因分析及对策
相关短句/例句
sustained torrential rain in South China华南持续性致洪暴雨
1.Using the daily and monthly NCEP/NCAR reanalysis data,Outgoing Longwave Radiation(OLR) data,monthly precipitation of 160 stations in China and daily precipitation of 45 stations in South China,relationships among sustained torrential rain in South China,anomalous convection over the Bay of Bengal and evolution of the western Pacific Subtropical High in June 2005 are analyzed.利用NCEP/NCAR再分析逐日及逐月资料、NOAA卫星观测的向外长波辐射(Outgoing Long-wave Radiation,OLR)资料、我国160站月降水资料及华南45站逐日降水资料,分析了2005年6月华南持续性致洪暴雨的发生与孟加拉湾对流异常活跃及西太平洋副热带高压演变的关系,并对华南6月有无持续性大范围暴雨年进行合成分析,结果表明华南持续性大范围暴雨发生的年份,孟加拉湾对流相对活跃,西太平洋副高强度偏强、位置偏西;反之亦然。
3)heavy rain over South of China华南致灾暴雨
4)flash-flood-producing rainstorm致洪暴雨
1.This paper carries out a numerical experiment on a flash-flood-producing rainstorm process from 3 to 5 September 2004 in Sichuan province,using NCEP/NCAR data and regional observational data as the background field.以NCEP/NCAR再分析资料和区域加密观测资料为背景场对2004年9月3—5日四川省一次特大致洪暴雨过程进行数值试验。
2.Based on the NCEP/NCAR daily reanalysis data,the circulation background of the flash-flood-producing rainstorm over South China in June 2005 and its possible cause are analyzed.利用NCEP/NCAR的逐日再分析资料,分析了2005年6月华南致洪暴雨的环流背景及其可能成因。
5)torrential rain致洪暴雨
1.Starting from the atmospheric circulation background and physical field diagnosis,and connecting with some meteorological observation data such as FY-2C nephogram and its products,this paper analyzes the geneses and characteristics of 7·29 torrential rain weather in Jincheng City,which provides the foundations for future forecast of torrential rain.从大气环流背景和物理量场诊断入手,结合FY-2C云图及其产品等探测资料,分析了晋城市"7·29"致洪暴雨的成因和特征,为今后预报致洪暴雨提供了依据。
6)flood rainstorm致洪暴雨
1.The results show that the flood rainstorm is closely related with lower level energy accumulation,a low-vortex shear line and the low-level jet on 700 hPa.应用天气学原理和方法,对1996年7月26~28日甘肃东部(渭河上游)暴雨过程的天气形势和物理量场的详细分析,结果表明,这次致洪暴雨的发生与低层能量的积累、700 hPa低涡切变和低空急流的形成有直接关系。
2.A contrast analysis on the course of two flood rainstorms along upper Weihe river is made.对渭河支流上游两次致洪暴雨过程进行了对比分析,结果表明:在泾河上游,两次大暴雨的落区相差在100km以内;两次暴雨过程均给当地和渭河下游造成了严重的洪涝灾害;洪水过程的洪峰特点分别属于缓型洪水和陡型洪水;500hPa天气分型虽然一次为西南气流型,一次为西风槽型,但700hPa的直接影响系统基本相同。
延伸阅读
华南前汛期暴雨华南前汛期暴雨rainstorm during pre-rainy season in South China hua’nan qianxunqi baoyu华南前汛期暴雨(rainstorm during Pre-rainy season in South China)每年4一6月发生在中国南岭以南地区(包括广东、广西和福建三省、区)的暴雨。华南地处亚热带，受夏季风影响较中国其他地区为早，3月末至4月初即进入汛期，4月至9月为暴雨季节，其中4一6月称为前汛期，这时产生暴雨主要为锋面、低空急流、切变线、低涡等温带天气系统;7一9月为后汛期，·暴雨主要由台风和东风波等热带天气系统所造成;华南前汛期多年平均暴雨日数可达4天以上，以5月最多，6月次之、4月最少。特大暴雨几乎都出现在5月和6月。暴雨中心与年雨量的多雨中心一致。在广西暴雨中心位于桂林附近的桂北地区，在广东省有3个暴雨中心;第一个在云开大山的迎风坡恩平、阳红附近;第二个在九连山的迎风坡清远、佛岗和龙门一带;第三个在粤东沿海和莲花山迎风坡一侧的潮汕平原一带。在福建暴雨中心位于闽北武夷山区。暴雨中心区，暴雨量约占全年降雨量的三分之一。前汛期暴雨过程短的不足1天。长的可达5一7天。华南地区降雨强度一般比内陆地区大得多，24小时暴雨量达100一200毫米比较常见，特大暴雨可达800毫米以上，暴雨过程总量可达1000毫米以上，前汛期暴雨是一次次冷暖空气交绥的结果。当东亚大气环流由冬季形势向夏季形势调整时，西太平洋副热带高压逐渐加强，西南和东南暖湿气流进入华南地区;由北方南下的冷锋移至华南趋于准静止状态，形成华南静止锋。高空西风槽在华南形成切变线，在锋后槽(切变线)前容易形成暴雨。地形作用促使华南前汛期暴雨中心多半集中于山脉的迎风坡。 (黄忠怒)
