1)heavy rainfall强降水
1.Comparison analysis on two heavy rainfalls in the east of Guanggong Province in July,2006;2006年7月粤东地区两次强降水过程对比分析
2.Analysis of a heavy rainfall weather process in the north of Ningxia Occurring宁夏石嘴山市一次强降水过程分析
3.Based on the successful diagnostic study,numerical simulation was conducted for better understand of heavy rainfall in lower latitude plateau from 0000 UTC 31 May to 0000 UTC 1 June 2001.对2001年5月31日~6月1日发生于低纬高原地区的一次强降水过程进行了数值模拟,在确定大尺度环流形势场、降水过程及雨团模拟正确的基础上,对引发强降水的主要雨团A,利用模式输出的高分辨模拟结果进行了深入的再诊断分析研究。
英文短句/例句
1.ANALYSIS ON YUNNAN SEVERE PRECIPITATION AROUSED BY CONVECTIVE CLOUD CLUSTERS OVER THE BAY OF BENGAL DURING EARLY SUMMER孟加拉湾云团影响下云南强降水分析
2.Mesoanalysis of Beijing Severe Precipitation in August 2008“080814”北京短时强降水过程中尺度分析
3.The analysis of short-time hard rain characteristics and its prediction methods study in Hangzhou杭州短时强降水特征分析及预报研究
4.Relationship Between ENSO and Frequency of Extreme Precipitation Days in China中国极端强降水日数与ENSO的关系
5.Changes of Flood-Season Severe Precipitation over South China in 2071-210021世纪末华南汛期强降水变化分析
6.Analysis of the Characteristics of Heavy Precipitation in Fangchenggang City in June of 2008防城港市2008年6月强降水特征分析
7.Analysis of a staged heavy precipitation caused by severe tropical storm一次强热带风暴引发的阶段性强降水分析
8.Analysed on a Heavy Precipitution in the Hinterland of Taklimakan Desert塔克拉玛干沙漠腹地一次强降水天气分析
9.NUMERICAL SIMULATION STUDY ON MCS OF A HEAVY RAINFALL PROCESS IN SOUTH CHINA一次强降水过程的中尺度对流系统模拟研究
10.A Mesoscale Analysis of Heavy Rainfall in Yunnan Caused by the Bengal Bay Depression孟加拉湾低压造成云南强降水的中尺度分析
11.Water reduces the potency of vodka.水能降低伏特加的强度。
12.precipitation of ice pellets when there are strong rising air currents.强上升气流造成的由冰粒构成的降水。
13.Heavy rainfall, and thus flooding, has increased.强降雨进而产生的洪水一直在增加。
14.Study on the Mobile Path and Rainfall of "0814" Typhoon Hagupit0814号强台风“黑格比”路径及降水分析
15.EVOLUTION OF PRECIPITATION INTENSITY IN DONGGUAN AND ANALYSIS OF TENDENCY IN RECENT YEARS东莞降水强度的演变及近年趋势分析
16.Analysis on the Phase Transformation of Precipitation During a Strong Cold Wave Happened in Spring一次春季强寒潮的降水相态变化分析
17.Diagnostic Analysis on the Track and Precipitation of Strong Typhoon Hagupit强台风黑格比的路径和降水诊断分析
18.Frequency and intensity of extreme precipitation events in China中国极端降水事件的频数和强度特征
相关短句/例句
Heavy precipitation强降水
1.Application of T213 Physical Quantity Field to Heavy Precipitation Forecasting;T213物理量场在强降水落区预报中的应用
2.Analysis of a staged heavy precipitation caused by severe tropical storm一次强热带风暴引发的阶段性强降水分析
3.A heavy precipitation weather was observed in Manxiyijing(83°06 E, 40°06 N ) on the hinterland of Taklimakan desert, from 23 - 24 Jllly, 1988.1988年7月下旬塔克拉玛干沙漠腹地满西异井测站出现了一次强降水天气，日降水量达28。
3)Heavy rain强降水
1.With the latest parallel version of regional climate model(RegCM3),three different cumulus convective parameterization schemes,Anthes-Kuo,MIT-Emanuel and Grell,are used to test their capability in simulating the heavy rain process happened in Yangtze-Huaihe River valley in July 2003.利用区域气候模式RegCM3的最新并行版本,选择Anthes-Kuo、MIT-Emanuel和Grell 3种积云参数化方案,对2003年7月发生在淮河流域的强降水过程进行了多组模拟试验,重点分析比较了3种参数化方案对降水总量分布、主要降水时段和基本气象要素场的模拟能力,并相对实测降水和要素场进行了统计检验。
2.A heavy rain occurred in Longyan on 18 June 2006 is analyzed by using the data of routine observation,automatic weather stations,satellite pictures, and CINRAD/SA observations.利用常规观测资料、自动站、卫星云图、雷达回波等资料对2006年6月18日龙岩强降水过程进行成因分析。
3.The cause of the heavy rainfall is analysed with the MICAPS data,GOES-9 satellite images.2004年8月23日在曲靖市境内出现了局地大暴雨的罕见强降水天气过程,出现了30年以来最大日雨量。
4)strong precipitation强降水
1.Starting from the requirement of railway flood-proof for the weather forecasting, this paper analyzes on the reasons of the generation of the railway flood disaster, probes into the influence of the strong precipitation on the railway line, and advances some precautions against the railway flood disaster.从铁路防汛对天气预报的需求入手,分析了铁路水害产生的原因,探讨了强降水对铁路线路的影响,并提出了对铁路水害的防范措施。
2.The result shows that there was no strong precipitation while the inverse trough north of Haitang moving across Hubei Province from east to west in the case of no secondary circulation,and there occurred strong precipitation while the inverse trough north of Talim moving across Hubei Province companying with the appearance of secondary circulations.结果表明:热带气旋"海棠"在西行过程中,其北部倒槽自东向西掠过湖北大部地区时,由于无次级环流出现,而未发生强降水天气;"泰利"在西行过程中,其北部倒槽在掠过鄂东地区时,由于有次级环流相配合,所以带来鄂东地区的强降水天气。
3.An extensive range and strong precipitation process happened from the night of July 29th 2003 to the morning of 30th in Shuozhou.同时,低层低涡、地面低压的发展触发了强烈的辐合上升运动,上层干冷、下层暖湿的不稳定层结也是这次强降水发生和维持的有利条件。
5)severe precipitation强降水
1.By using the data of new generation radar precipitation model production and relevant weather maps,real-time precipitation data during May and September in 2004,2005,this paper analyzed and studied the intensity and range of radar echo,the velocity and direction of movement about different kinds severe precipitation on single cases of severe precipitation in Urumqi.利用乌鲁木齐市2004年和2005年的夏半年(5月至9月)新一代雷达降水模式的产品资料及相应的天气图、实时降水量等资料,对乌鲁木齐市强降水个例的降水时雷达回波强度和范围、不同类型性质降水的移速及移向进行了分析研究。
2.The results show that the track of Winnie is to the east,its increment of moving velocity is bigger after turning,and the precipitation over Liaodong Peninsula is larger;The track of Tim is to the west,its enhancement of moving velocity is smaller,and the center of severe precipitation is in North China.选取移动路径和转向趋势极为相似的两个热带气旋——9711(Winnie)和9406(Tim)为例,对其路径、降水量、移动速度进行对比分析,结果表明,Winnie路径偏东,转向后移动速度增幅大,在辽东半岛地区的降水量大;Tim路径偏西,转向后移动速度增幅小,强降水偏西。
3.Results show that the very stiff moist isentropes can lead to the development of moist slantwise vorticity and the severe precipitation may occur there;conditionally symmetric instability is another important factor responsible for this severe precipitation;the weak atmospheric stability and strong baroclinicity are favourable to the happening of severe winter precipitation over Yunnan.应用倾斜涡度发展理论，对云南的一次冬季强降水天气进行诊断分析。
6)precipitation intensity降水强度
1.Based on the daily precipitation records of 10 selected stations over 1951-2001 period,the climatic variations,tendencies of yearly and seasonal precipitation amount,precipitation days and precipitation intensity in Mid-Lower Yangtze River valley during last 51 years are investigated with least square linear fitting method.利用1951-2001年10个代表站的逐日降水观测资料,运用线性趋势法分析了51年来长江中下游地区年和季的降水量、降水日数和降水强度的变化趋势,用Mann_Kendall法对降水日数和降水强度的突变进行了检验,并对日降水量分级别讨论了各等级对总降水量贡献的变化趋势。
延伸阅读
椐椐强强1.相随貌。
