1)pre-flood汛前
1.According to historical hydrologic data,under current electricity price,the control of the regressing of the pre-flood water level of the Wuqiangxi Reservoir is analyzed with dynamic programming theory.采用历史水文资料,在当前丰枯电价条件下,运用动态规划理论,分析归纳五强溪水库汛前库水位控制规律,提出了五强溪水库汛前消落方式及产生的效益。
英文短句/例句
1.Study on Operation Optimization in Pre-flood Falling Stage of the Three Gorges Reservoir三峡水库汛前消落期优化调度方式研究
2.Regressing Mode Analysis of Pre-flood Water Level for Hunan Wuqiangxi Reservoir湖南五强溪水库汛前水位消落方式分析
3.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
4.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
5.Before the flood season comes, we must rush to build the dam.在洪汛期到来之前, 我们必须要抢建大堤!
6.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
7.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
8.Analysis on the Pre-flood Season Sustained Rain Process of Southern China in 20082008年华南前汛期连续性暴雨过程成因探析
9.The Difficulties of Current Flood Control Work in Yulin and the Countermeasures玉林市当前防汛工作的难点与应对措施分析
10.The Comparative Analysis of Precipitation Variations during the First and Second Flood Season in Chaozhou by Wavelet Analysis潮州市前、后汛期降水量的多时间尺度特征对比
11.The Setting and Influence of Tang Xun in Tibetan Kham Area in the Early Qing Dynasty清代前期康区塘汛的设置及其作用与影响
12.SVD ANALYSIS BETWEEN THE ANNUALLY FIRST RAINING PERIOD PRECIPITATION IN THE SOUTH OF CHINA AND THE SST OVER OFFSHORE WATERS IN CHINA华南前汛期降水与我国近海海温的SVD分析
13.ANALYSIS OF PRECIPITATION IN THE ANNUALLY FIRST RAINY PERIOD AND GENERAL CIRCULATION IN THE SOUTH OF CHINA华南前汛期降水异常及其环流特征分析
14.Before the arrival of the flood season, everybody was ready to fight floods and reduce damage.在洪汛期到来之前, 大家早已做好了抗涝减灾准备。
15.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
16.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
17.The Space-time Distribution of Rain During Former Flood Season and Its Relationship with the East Asian Monsoon;福建省前汛期降水时空分布特征及其与东亚冬季风的关系
18.Features of the Precipitation during the Pre-Flood Season in South China and It s Interaction with South China Sea Summer Monsoon;华南前汛期降水特征及其与南海夏季风的相互作用
相关短句/例句
pre-rainy season前汛期
1.The regional durative rainstorm during pre-rainy season over South China is defined and its climatic distribution features before and after the onset of South China Sea summer monsoon are studied using daily rainfall data of 175 stations in Guangdong and Guangxi provinces.利用广东和广西两省共175个台站的日降水观测资料,采用计算机检索的方法,对1961-2005年间华南前汛期区域持续性暴雨进行了定义。
2.Following Part I of this study,spatial patterns of frontal rain and summer monsoon rain during pre-rainy season in South China are explored in this paper.利用中国730站降水资料和第I部分(郑彬等,2006)得到的华南前汛期锋面降水和季风降水的划分日期,计算出1958-2000年华南前汛期锋面降水量(强度)和季风降水量(强度)的序列,采用EOF和扩展EOF分析方法,得到华南前汛期降水的几个主要分布型,并探讨锋面降水与季风降水的可能联系。
3.Following the Part I, spatial patterns of frontal rainfall and summer monsoon rainfall during pre-rainy season in South China were explored in this paper.利用中国730站降水资料和第I部分得到的华南前汛期锋面降水和季风降水的划分日期,计算出1958-2000年华南前汛期锋面降水量(强度)和季风降水量(强度)的序列,采用EOF和扩展EOF分析方法,得到华南前汛期降水的几个主要分布型,并探讨锋面降水与季风降水的可能联系。
3)pre flood period前汛期
1.Through the EOF analysis method and Z index,kenel distribution of precipitation as well as flood and draught level in the pre flood period(April~June) are graded with a view to study the spatial distribution,annual changes and changes in decades of flood and draught,and an analysis for the causes of flood and draught is also made.利用 EOF分解和 Z指数对广西前汛期 (4～ 6月 )降水进行型态分布及旱涝等级的划分 ,研究旱涝的空间分布、年际变化及年代际变化 ,并对旱涝成因进行了分析。
4)rain period前后汛期
5)prefreshet period汛前期
6)pre-flood seasonal heavy rainfall前汛期暴雨
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 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)
