1961-2007年陕西省极端降水事件的时空演变

Q3 Environmental Science 干旱区研究 Pub Date : 2011-01-01 DOI:10.3724/sp.j.1148.2011.00151
Hui Ying
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引用次数: 0

摘要

利用陕西省78个气象站1961—2009年逐日观测的降水资料,分析了极端降水事件的时空变化特征。结果表明:极端强降水阈值在18.7 ~ 9.5 mm/d范围内变化,向北减小;全省极端降水事件主要发生在5 - 9月的雨季,特别是7 - 9月,持续时间以1天为主,2天的极端降水事件主要发生在陕南中南部,3天的极端降水事件偶有发生。近49 a来,全省年极端降水事件变化趋势不显著,但夏季极端降水事件有所增加。EOF分析结果表明,浙江省极端降水事件发生频率存在两种主要的空间分布格局。第一种(EOF1)是全省极端降水事件的高、低频率基本一致,存在22 a和准8 a的周期变化。②EOF2为东南部与西北部极端降水事件发生频率相反,存在12-14 a和2-3 a的周期变化。
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Spatiotemporal Evolution of Extreme Precipitation Events in Shaanxi Province during the Period 1961-2007
In this paper,the spatiotemporal change of annual extreme precipitation events is analyzed using the daily precipitation data observed by 78 meteorological stations in Shaanxi Province during the period 1961-2009. The results show that the threshold of extreme intensity precipitation varied in a range of 18.7-9.5 mm/d,and it decreased northward. The extreme precipitation events in the province occurred mainly in rainy season from May to September,especially during the period from July to September,their duration was mostly for one day,the extreme precipitation events with 2-day duration occurred mainly in the central-southern part of south Shaanxi Province,and those with 3-day duration were occasional. The change trend of annual extreme precipitation events in the province was not significant in recent 49 years,but the extreme precipitation events increased in summer. The EOF results reveal that there were 2 main spatial distribution patterns of frequency of extreme precipitation events in the province. The first one (EOF1) was that the high or low frequency of extreme precipitation events was accordant in whole province,and there were 22-year and quasi-8-year periodic changes. The second one (EOF2) was that the frequency of extreme precipitation events in the southeastern part was opposite to that in the northwestern part,and there were the 12-14-year and 2-3-year periodic changes.
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来源期刊
干旱区研究
干旱区研究 Environmental Science-Water Science and Technology
CiteScore
2.50
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0.00%
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4294
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