汛期暴雨,flood season rainstorm
1)flood season rainstorm汛期暴雨
1.The 1960- Nanjing Countyflood season rainstorm climate diagnosis indicated that the firstflood season rainstorm mainly concentrated in late May to mid-June.对1960-南靖县汛期暴雨气候分析表明,前汛期暴雨主要集中在5月下旬-6月中旬,后汛期暴雨主要出现在8月上旬、8月下旬和9月上旬。
2.By using the rainstorm data in the 1990~ period,the distribution of theflood season rainstorm in Henan province is studied.利用1990~河南暴雨资料,分析了河南汛期暴雨空间分布特征,结果表明:豫西山区暴雨日最少,省内淮河流域暴雨日最多,豫北暴雨日次多。
英文短句/例句
1.The Space-time Change of Rainstorm and Origin Cause of Formation in Pre-Summer Flood Period of South China;华南前汛期暴雨的时空变化及其成因
2.Water Vapor Analysis of Heavy Rain Events in Guangxi in July 7月广西汛期暴雨过程水汽特征
3.Study on the Mechanism of Early-Summer Rainstorms in Southern China Triggered by Tropical Disturbances;热带扰动引发华南前汛期暴雨的机理研究
PREHENSIVE ANALYSIS ON CLIMATIC CHARACTERISTICS AND FORECAST METHODS OF HEAVY RAINFALL IN JIANGXI DURING FLOOD-SEASON江西省汛期暴雨气候特点及预报方法综合分析
5.Analysis on Large-Scale Circulation Characteristic of Meiyu Rainstorm and Structure of Meiyu Front in Zhejiang Province during 浙江梅汛期暴雨的大尺度环流特征及其梅雨锋结构分析
6.Frequency Characteristics of Rainstorms in Flood Season of Guangxi and Correlation to the Onset Time of South China Sea Summer Monsoon广西汛期暴雨特征及其与南海夏季风建立期的关系
7.The Cause Analysis and Numerical Simulation of a Rainstorm of South China in the First Rainy Season;一次华南前汛期暴雨的成因分析及数值模拟研究
8.Heavy Rainfalls in South China and Related Circulation during First GARP Global Experiment Period第一次全球大气研究计划试验期间华南前汛期暴雨过程及其环流特征的诊断研究
9.The strong forecast signals for torre ntial rain process in Guangdong have been given by the approaches of synthesizin g High and Low Latitude Circulation Indices, Australia High Index and South Westerly Trough Index.从高低纬环流指数、南支槽指数和澳洲高压指数，综合得到广东汛期暴雨过程的强信号。
10.Analysis of Meteorological Factors of Regional Heavy Rainfall in East China during Meiyu Period;华东梅汛期分片暴雨前期气象因子场的分析
11.Analysis on the Pre-flood Season Sustained Rain Process of Southern China in 华南前汛期连续性暴雨过程成因探析
12.Numerical Simulation and Analysis on a Heavy Rain Process in the Warm Sector in Guangxi广西前汛期锋前暖区暴雨过程的模拟与分析
13.TBB Features of Continuous Torrential Rain over Huaihe River Valley in Summer of 汛期淮河流域连续性大暴雨TBB场分析
14.Numerical Simulation and Diagnostic Analysis of a Warm Sector Rainstorm Occurring in Guangxi Province Area;广西前汛期暖区特大暴雨MCC的数值模拟与诊断研究
15.A Case Study of Continuous Torrential Rain in Guangdong during the Pre-flood Period in 广东前汛期一次连续性特大暴雨的特征及成因
16.depth-area-duration analysis of severe rainstorm暴雨的雨量─面积─降雨期分析
17.Study on the Urban Flood-control Decision Support System for the Storm Water Logging Disaster;针对暴雨积水灾害的城市防汛决策支持系统研究
18.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
相关短句/例句
pre-flood seasonal heavy rainfall前汛期暴雨
3)rainfall in flood period汛期降雨
4)flood season rainfall汛期雨量
1.The research of the inter-decadal abrupt turning of theflood season rainfallin Yunnan Province;云南汛期雨量年代际转折突变的研究
5)Precipitation Pattern of Flood Period汛期雨型
6)rainstorms during the Meiyu period梅雨期暴雨
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 Chinahua’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)
