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1)  cold and rainy weather of spring
春季低温阴雨
1.
Based on the daily mean temperature of 8 stations between late February and April in Shaoguan during 1965-2004,the statistics methods were applied to research the climatic variations of cold and rainy weather of spring in Shaoguan;The results of analyses reveal: in Shaoguan region,there were 8-14d\'s cold weather every year on average,and most of which were going with rain.
对1965~2004年韶关市的春季低温阴雨日数进行统计分析,结果表明,韶关市的低温阴雨年平均日数在8~14 d,大部分都是湿冷型。
2)  low temperature and continuous rain in spring
春季低温连阴雨
3)  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。
4)  Spring low temperature
春季低温
5)  cold and rainy weather
低温阴雨
1.
By using the temperature and sunshine data(1959-2008)of Foshan and so on,the causes and climatic fea- tures of a rare cold and rainy weather in Foshan in early 2008 are investigated.
基于佛山市1959~2008年气温和日照等资料,分析佛山2008年初罕见低温阴雨的成因及低温阴雨的气候特征,结果表明:2008年低温阴雨属于异常天气气候事件。
6)  continuous cold rainy days
低温连阴雨
1.
The decadal changes of the continuous cold rainy days in spring denote that there are less days than climate average during the 1950s and from 1997 to present,and the temporal variations of the first EOF mode of the continuous cold rainy days of China show the characteristics of decade oscillations including inter-month seesaw during the period of 1963—1996.
利用1951—2007年2—5月我国546个站逐日平均气温和24 h降水量观测资料以及南方早稻区代表站日照时数观测资料,定义了全国统一的低温连阴雨标准和早稻区低温冷害标准,并采用统计分析方法,给出了1951 2007年2—5月我国低温连阴雨和低温冷害的时空变化特征。
补充资料:春季
1.一年第一季。即从立春至立夏的三个月时间。习惯上亦指农历正﹑二﹑三三个月。
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