特大暴雨

  • 网络extraordinary storm;rainstorm;heavy rainfall
特大暴雨特大暴雨
  1. 贺江流域特大暴雨洪水特性分析

    Analysis of extraordinary storm flood characteristics of Hejiang river basin

  2. 副高控制下鹤壁局地特大暴雨过程分析

    Analysis of Local Extraordinary Storm Process Controlled by Subtropical High Over Hebi

  3. 上海0185特大暴雨的MCS形成条件分析

    Analysis of MCS ′ Evolving Condition in 0185 Torrential Rainstorm of Shanghai

  4. 一次中尺度对流系统(MβCS)触发特大暴雨机理研究

    Triggered Mechanism Analysis of an Meso - β scale Convective System ( M_ β CS ) on Heavy Rainfall

  5. 同时,用非地转湿Q矢量分析方法诊断了由北上台风倒槽引起的一次华北特大暴雨过程;

    At the same time , the non geostrophic wet Q vector was applied to diagnose a torrential rain process in North of China .

  6. 引发湖南特大暴雨山洪的MCS回波发展和演变

    Development and evolution of the radar echo of MCS in Super Heavy Rain Flush Flood

  7. 低纬高原地区2008年7.02特大暴雨MβCS结构特征的数值模拟分析

    Numerical modeling analysis on M_ β CS structure characteristics of " 7.02 " heavy storm rainfall event which happened in 2008 in lower latitude plateau

  8. OLR资料在华南前汛期特大暴雨过程分析和预报中的应用

    Application of OLR data in analysis and forecast of exceptionally heavy rain in April-June rainy season in South China

  9. 结果显示,在洪水来临以前,发生过两次特大暴雨,并伴有冰层融化,土壤饱和,高地下水等现象。通过对比,科学家发现,与现有的洪水预警仪器相比,GRACE卫星可以提前数月据预测出洪水的发生。

    Preceding the flood were two significant storms , record snow melt , saturated soils and particularly high groundwater.With GRACE data , the researchers found that they could have predicted the Missouri River floods months before current prediction models .

  10. 对2003年7月9日至10日发生在我国长江流域的一次特大暴雨天气过程用MM5模式进行了数值模拟。

    Experiments for the case of the rainfall occurred in the Changjiang River during 9-10 , July , 2003 , are carried out .

  11. 1998年7月20~23日(简称98.7)发生在武汉周边地区的特大暴雨过程与沿低涡切变线相继生成和强烈发展的MαCS及MβCS直接关联。

    During the period of 20 ~ 23 July 1998 (" 98.7 " ), an extraordinary heavy rainstorm event occurred in Wuhan surrounding which was direct relationship with the successive generating and intensive developing M α CSand M β CS .

  12. 结果表明:高、低空急流耦合区中西南低涡及MCC特征云团的形成和维持是造成此次特大暴雨的直接影响系统。

    The results show that the event is directly affected by the formation and evolution of southwest vortex and MCC cloud cluster which locate in the intersection region of the upper-level jet and the low-level jet .

  13. 本文利用改进了水汽输送方案的中尺度模式MM4对三次暴雨过程作了试验,这三次过程包括两次长江中下游特大暴雨和一次华北暴雨。

    In this paper , the moisture transport algorism of mesoscale model MM4 is improved by adding positive definite moisture transport schemes with high accuray .

  14. 利用改进的有限区域数值预报模式(AREM),对“艾利”台风在福建省登陆所造成的特大暴雨过程进行了数值模拟;

    A heavy storm rainfall , caused by Typhoon " AERE " when landing at Fujian , has been successfully simulated by using AREM model .

  15. 研究9012号台风(YANCY)中尺度螺旋雨带结构特征及其与闽东北沿海地区特大暴雨的关系。

    This paper is to analyse the structure of the mesoscale rotational rain belt of Typhoon 9012 ( YANCY ) and its relationship with the heavy rainfall in north east of Fujian .

  16. 使用10分钟间隔的武汉WSR-81S数字化雷达回波资料,结合逐时地面风场及雨量,对1998年7月20~21日出现在湖北省东部的特大暴雨过程进行了详细的中尺度分析。

    Using ten minute WSR 81S digital radar echo data , together with hourly wind and rainfall data , the extremely heavy rain occurring in East Hubei Province in 20 ~ 21th July 1998 is analyzed .

  17. “98.7”特大暴雨过程与700hPa低涡切变线的强烈发展以及丰沛的水汽和强垂直运动密切相关。

    The " 98.7 " extraordinary heavy rainfall event was in close relationship with the intensive development of a low vortex with shear line on 700 hPa and the abundant moisture as well as strong vertical motion .

  18. 使用MUSCAT技术对这次特大暴雨进行了双多普勒雷达三维风场反演,研究表明,中低层辐合线和中尺度气旋是造成此次暴雨的重要原因;

    The three-dimensional wind of the heavy rain were retrieved by MUSCAT ( multiple-Doppler synthesis and continuity adjustment technique ) using the dual-Doppler radar volume scan data . It showed that the convergence line and the meso-cyclone at the low level play an important role in this heavy rain event .

  19. 双向嵌套的细网格模拟结果揭示,武汉周边地区的特大暴雨与700hPa上一个β中尺度低涡的生成和强烈发展直接关联。

    The simulated results using two-way interactive fine grid reveal that . the extraordinarily heavy rainfall in the Wuhan periphery was in direct relationship with the genesis and intensive development of a meso - β scale low vortex at 700 hPa ;

  20. 利用WSR88D多普勒雷达资料,通过分析2001年8月5日到8月6日产生于上海地区的特大暴雨过程的雷达回波特征,研究探讨这次过程的降水成因和降水特点。

    Based on WSR 88D radar data , the radar echo ′ s characteristics of the torrential rain in Shanghai on the night of August 5th 2001 are analyzed to find out its precipitation mechanism and characteristic .

  21. 对2002年6月8日发生在陕西佛坪的一次特大暴雨过程进行了综合分析,结果表明:500hPa槽前的中尺度切变线是直接影响暴雨产生的中α尺度系统;

    Systematically analyses were carried out for an abrupt heavy rainstorm in Fuping of Shaanxi province on June 8 , 2002 . The results show that a meso-scale shear line lying in front of 500 hPa trough is the meso - α - scale system that causes the rainstorm .

  22. 川北两次特大暴雨天气过程成因的对比分析

    Contrast Analysis of Two Heavy Rain Cases over Northern Sichuan Basin

  23. 梧州市6.8灾害性特大暴雨分析

    Analysis of the " 06.08 " Severe Rainstorm in Wuzhou City

  24. 一次罕见的特大暴雨物理量场特征分析

    Physical Features Analysis of a Rare Torrential Rain in the Land

  25. 温州9909热带风暴外围特大暴雨分析

    Study of Wenzhou Abnormal Heavy Rain Associated With 9909 Tropic Cyclone

  26. 一次地形引起的特大暴雨雨量增幅过程分析

    An Analysis of The Extraordinary Heavy Rainfall Increment Process Of Orographic

  27. 2004-07-16河南省特大暴雨过程螺旋度分析

    Helicity Analysis on the Torrential Rain in Henan in July 16,2004

  28. 2005年10月平阳一次台风特大暴雨天气过程分析

    Analyses of a Heavy Rain in Pingyang City on October 3,2005

  29. 深圳河流域6.13特大暴雨洪水特性分析

    Flood Characteristic Analysis of 6.13 Super Rainstorm in Shenzhen River Valley

  30. 塔里木盆地一次特大暴雨过程的分析

    A Case Analysis of Torrential Rain in Tarim Basin in Xinjiang