2) storm intensity
暴雨强度
1.
Immune evolutionary algorithm and its application to parametersoptimization in storm intensity formula;
免疫进化算法及其在暴雨强度公式参数优化中的应用
2.
A Statistical method of city storm intensity formulas;
城市暴雨强度公式的统计方法
3.
By utilizing hydrology, climatology, geomorphology, computer and GIS technology, measured data on the annual rainfall of 824 stations in the Hangzhou region were collected, and the formula of storm intensity in 23 rainfall stations was ascertained.
运用水文学、气候学、地貌学、计算机和GIS技术,采集了杭州地区824站的年降水实测资料,推求出了23个雨量站的暴雨强度公式,对整个杭州市的设计暴雨强度空间分布进行了深入研究。
3) rainstorm intensity
暴雨强度
1.
A study of the formula of rainstorm intensity in Handan city;
邯郸市暴雨强度公式研究
2.
Research on a new-generation of rainstorm intensity formula for Shenzhen City;
深圳市新一代暴雨强度公式的研制
3.
The parameters of nine duration rainstorm intensity samples must be estimated when formulating the rainstorm intensity in urban drainage engineering.
城市排水工程中编制暴雨强度公式时,须对九种历时暴雨强度的样本系列进行参数估计。
4) strong dust storm
强沙尘暴
1.
A medium-range synoptic analysis of Strong dust storm on 12 April 2000;
“4.12”强沙尘暴天气中期分析
2.
In this paper,the dustfall characteristics during the period from April to June and the strong dust storm events in a zone sheltered by 24-year-old artificially afforested forest of Populus simonii for sand fixation over the Horqin Sandland are studied by measuring some parameters of dustfall at some field stationed observation sites.
采用野外定位实测法,连续两年对科尔沁沙地24龄人工固沙杨树(Populussimonii)林庇护区内4～6月份及强沙尘暴事件中的降尘特征进行了观测研究。
3.
By using the reanalysis data of NCEP(1°×1°),the dry intrusion characteristic of a strong dust storm process occurred in the Hexi Corridor from April 9 to 10,2006 was analyzed.
使用NCEP(1°×1°)每天4次的再分析资料对2006年4月9~10日发生在甘肃省河西走廊的一次强沙尘暴天气进行了诊断分析。
5) Severe storm
强风暴
1.
The methods for diagnosing severe storm potential are studied accordingly in combination with the fuzzy logic method.
利用中尺度数值预报模式,计算、输出若干与强风暴发生发展有密切关系的常规物理量和对流参数,研究应用模糊逻辑学技术的强天气潜势诊断的方法,开发出雷暴、冰雹、雷雨大风3类对流性天气落区的潜势预报产品,并进行了初步的业务试验。
2.
A severe storm happened around the Three Gorges Dam area at midnight on 15 April 2002,which is the typical convective weather occurred under the condition that the cold front invades into the southwest inverted trough.
2002年4月15日夜间发生在三峡坝区的强风暴属于典型的地面冷锋侵入西南倒槽天气背景下的强对流过程,其瞬间最大风力达11级,降水强度达50 mm/h左右。
3.
Based on the synthetical analysis of lightning data and Doppler radar echoes from a severe storm event in Henan Province on 19 June 2003, relationship is found between lightning frequency and radar echo intensity.
根据2003年6月19日河南一次强风暴天气的闪电定位资料和714CD雷达资料,利用统计和对比分析的方法,发现了闪电活动与雷达强度回波之间存在如下关系:闪电发生频数、强度和雷达回波强度在时间序列上有较好的一致性;在雷达回波发展的不同阶段,闪电发生的位置与雷达强回波位置有时相同,有时偏离,有时甚至无闪电发生;雷达回波速度场分析表明:在低层存在不利于对流发展的环境风场特征时,雷达降水回波在向测站移动的过程中趋于消散,闪电频数也随着减少;在降水回波速度辐合区,对应闪电活动频繁,这对于雷暴天气闪电短时预警工作有一定的参考价值。
6) strong sandstorm
强沙尘暴
1.
This paper researched the characteristics and causes of strong sandstorms invading the middle area of Gansu through analyzing the weather system by using the high and surface data from 1970 to 2006.
利用1970—2006年甘肃中部13个县(市)的21例沙尘暴天气过程的各时次高空和地面资料,通过分析沙尘暴过程的影响系统,来研究甘肃中部近年来强沙尘暴天气频繁入侵的成因及特点。
2.
The strong sandstorm and cold wave weather process were occurred from the west toward the east in Hetian area during Apr.
2006年4月9日20时开始,和田地区自西向东出现了强沙尘暴、寒潮天气过程。
3.
The high-circumfluent pattern of strong sandstorm in Gansu province from 1995 to 2002 was analyzed by using the high and surface meteorological data.
利用探空、地面资料分析了1955—2002年甘肃省发生强沙尘暴天气的环流特征,揭示出甘肃沙尘暴天气的5种环流类型:冷锋后偏西型、强锋区下动量下传型、冷高压南部型、热低压前部型和河西小槽型的平均环流场特征。
补充资料：强暴
强横凶暴：强暴势力｜强暴的日寇。也指强暴的势力、行为：反抗强暴｜施行强暴｜背故君而事强暴，可谓忠乎?
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条