1)Continuous rain连阴雨
1.Analysis and Forecast of Continuous Rain over Jiaozuo;焦作市连阴雨天气分析与预报
2.Analysis of Climate Characteristics of Continuous Rain in Binzhou City,Shandong Province近47年山东省滨州市连阴雨气候特征分析
3.Using the summer hourly rainfall data of 3B41RT from TRMM(Tropical Rainfall Measuring Mission) satellite of 2002~2006,taking continuous rain,storm and daily rainfall series as examples,the TRMM satellite s capability for detecting summer rainfall in Shaanxi and its neighborhood regions is analyzed by comparing the rainfall data from TRMM satellite with the data from ground weather stations.采用2002~2006年夏季6~8月热带降水测量(TRMM)卫星3B41RT类数据资料,以发生在陕西及周边地区的连阴雨、暴雨和日降水量序列事件为例,通过比较TRMM卫星降水资料与地面气象站观测资料的差异,分析了TRMM卫星对陕西及其周边地区夏季降水过程的探测能力。
英文短句/例句
1.The Research of Forecast Models for Continuously Cloudy or Rainy Weather Based on Matlab Neural Network基于Matlab神经网络连阴雨预报模型研究
2.Analysis of Water Vapour Transport in the Upper Yellow River during Continuously Heavy Rain of August and September 19811981年8～9月黄河上游强连阴雨期水汽输送分析
3.Comparatice analysis on local heavy rain in spring and autumn continue rainfall process罕见春秋季连阴雨过程局地强降水的对比分析
4.Analysis of an Infrequent Continuous Rain Weather Process in Autumn in Northwest China西北地区一次罕见的秋季连阴雨特征分析
5.Analysis of a Rare Continuous Autumn Rain in Northwest Shandong鲁西北罕见的秋季连阴雨环流特征分析
6.Analysis of Climate Characteristics of Continuous Rain in Binzhou City,Shandong Province近47年山东省滨州市连阴雨气候特征分析
7.The Spatial and Temporal Characteristics of China Continuous Cold Rainy Weather and South Cold Damage from February to May2—5月我国低温连阴雨和南方冷害时空特征
8.Diagnostic Analysis of a Glaze Weather Process in the Context of Low Temperature and Persistent Rainy (Snowy) Days in the Central Region of Zhejiang Province低温连阴雨(雪)背景下浙中一次雨凇天气过程诊断分析
9.Characteristics of Circulation and Moisture Flux During a Continuous Autumn Rain Process in 2008 in Yunnan Province2008年云南省秋季连阴雨天气的环流及水汽特征分析
10.Law of Autumn Continuous Precipitation Occurrence and its Influence on Autumn Harvesting and Planting in Anhui Province安徽省秋季连阴雨发生规律及对秋收秋种的影响
11.It has been cloudy and drizzly for days on end.近几天一直阴雨连绵。
12.I'm sick of this constant rain.我讨厌这连绵阴雨。
13.Continual rain ruined the crops.连续阴雨毁坏了庄稼。
14.It is settling in to rain now.现在要阴雨连绵下个不停了。
15.But in the Midwest, you may expect a lot of rain.可是中西部很可能阴雨连绵。
16.This continual wet weather is getting me down.连绵的阴雨天气使我感到毫无精神。
17.Continuous rain prevented us from taking any outdoor exercise.阴雨连绵，使我们不能做任何室外运动。
18.it is finally sunny after the continuous rain.连绵阴雨后, 终于又见到了晴空!
相关短句/例句
Cloudy-rainy Weather for several days连阴雨
1.The study shows that: (1) Cloudy-rainy weather for several days in Zhejiang tends to increase from North to South.研究了 3月中旬～ 5月上旬浙江省双季早稻育秧期长、中、短连阴雨的时空分布规律 ,以及年代间演变规律。
3)continuous overcast rain连阴雨
1.From September 27 to October 11 in 2007,there was a continuous overcast rain weather which was rare in history.分析了2007年9月27日10月11日长治市出现的历史罕见的持续时间最长、影响范围最广、灾害最严重的秋季连续阴雨天气的成因,给出了秋季连阴雨的预报着眼点:副高脊线位于25°N以北、西伸脊点位于110°E,北部冷空气南下受副高阻挡,在40 55°N形成平直西风带锋区,锋区南侧偏西西北气流与副高边缘西南气流交汇,切变系统频频建立,是山西中南部连阴雨天气的产生机制。
2.Based on the data of the upper air chart,the surface intensive observation and variety of the physical parameter field,we analyze the process of the continuous overcast rain occurred in deep autumn in 2006 in Puyang.利用高空天气图、地面加密观测、多种物理量场等资料,分析了2006年深秋发生在濮阳市的连阴雨天气过程,结果表明:500 hPa大尺度环流形势稳定,有利于中低层中尺度系统的形成,为本次降水过程提供了动力机制;500 hPa横槽不断有冷空气扩散南下,在中纬度地区产生小波动,每一个小波动与暖湿气流在濮阳市交汇,配合700 hPa低槽、切变线及地面中尺度辐合线共同作用造成了持续的阴雨天气;地面气压场上东南沿海气旋波北扩到35°N,既为降水过程提供了水汽和能量供应,也阻止了北方冷空气的快速南下,使冷、暖空气在濮阳市汇合;物理量场的变化,对这次连阴雨的预报有一定的指示意义。
4)There was an unbroken spell of wet weather.阴雨连绵。
5)spring continuous rain春季连阴雨
1.The relationship between SST field of the Pacific and spring continuous rain (or cloudy-rain weather for several days)in Jiangsu Province was discussed.对江苏春季连阴雨和太平洋海温场的关系进行研究,发现二者相关显著。
6)the persistent rainy processes in spring春李连阴雨
延伸阅读
连阴雨连阴雨中国初春或深秋时节接连几天甚至经月阴雨连绵、阳光寡照的寒冷天气。又称低温连阴雨。连阴雨同春末发生于华南的前汛期降水和初夏发生于江淮流域的梅雨不同。后两者虽在现象上也可称连阴雨，但温度、湿度较高，雨量较大；而前者的主要特点是温度低、日照少、雨量并不大。连阴雨的灾害，主要在低温方面。初春连阴雨，往往出现在水稻播种育秧时节，易造成大面积烂秧现象；秋季连阴雨如出现较早，会影响晚稻等农作物的收成。连阴雨天气就产生在地面锋和700百帕等压面的切变线之间。春季，中国南方冷暖空气交绥处（即锋）经常停滞或徘徊于长江和华南之间，当锋面和切变线的位置偏南时，连阴雨发生在华南；偏北时，就出现在长江和南岭之间的江南地区。秋季的连阴雨，其过程与春季相似，只是冷暖空气交绥的地区不同，因而连阴雨发生的地区也和春季有所不同。
