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摘要:
Continuous rainy and cold weather in Yiwu in early spring of 2009 was analyzed.The results showed that the continuous rainy and cold weather occurred after temperature increased in early days.It is mainly because that the high geopotential height near Ural Mountains lasted for a long time,while the geopotential height was abnormally low in the east of central Asia.Meanwhile,the low-pressure trough in the south of Qinghai- Tibet Plateau was very active and moved towards the east frequently,and subtropical high was strong.Compared with continuous rainy and cold weather in early 2008,during the process of this continuous rainy and cold weather in 2009,the decrease in sea surface temperature of the middle and eastern Pacific Ocean near the equator was weaker;the blocking high pressure was slightly weaker,and the low pressure over Mongolia was strong;subtropical high was stronger and showed zonal distribution;south trough was slightly weaker.Compared with the previous continuous rainy and cold weather,the duration of this continuous rainy and cold weather in 2009 was not the longest,and its sunshine hours were not the least,but its temperature was higher,which might result from obvious increase of temperature in the early days.The research could provide scientific references for the prediction of continuous rainy and cold weather in future.
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篇名 Analysis of Continuous Rainy and Cold Weather in Yiwu in Early Spring of 2009
来源期刊 气象与环境研究:英文版 学科 地球科学
关键词 寒冷 阴雨 天气 春分 温度升高 青藏高原南部 持续时间 乌拉尔山脉
年,卷(期) 2014,(1) 所属期刊栏目
研究方向 页码范围 20-23
页数 4页 分类号 P457.6
字数 语种
DOI
五维指标
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参考文献  (22)
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研究主题发展历程
节点文献
寒冷
阴雨
天气
春分
温度升高
青藏高原南部
持续时间
乌拉尔山脉
研究起点
研究来源
研究分支
研究去脉
引文网络交叉学科
相关学者/机构
期刊影响力
气象与环境研究:英文版
双月刊
2152-3940
出版文献量(篇)
1887
总下载数(次)
1
总被引数(次)
0
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