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气象:2006,32(9):90-94
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抚顺冬季异常偏冷年气候特征及成因分析
(1.南京大学大气科学系, 210093;2.辽宁省抚顺市气象台;3.沈阳区域气象中心)
Analysis of Climatic Characteristics and Causes of Anomalous Cold Winter in Fushun, Liaoning
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投稿时间:2005-11-29    修订日期:2006-05-09
中文摘要: 利用抚顺气象观测站气象资料,分析了抚顺冬季异常偏冷年的气候特征,发现异常偏冷年都有最低气温低于-30℃的冷段,并且气候变暖后,降雪多、积雪深是其主要特征。同时通过分析深层平均地温、太阳黑子活动、大气环流等资料,发现抚顺冬季气温异常偏低一般都出现在太阳黑子峰谷年附近,并与前期3—11月0.8m深层平均地温呈正相关,北半球500hPa冬季欧亚地区距平场为西高东低,东亚槽稳定建立,并且大气环流以大西洋-欧亚E型环流型为主。
Abstract:Based on the data from weather stations in Fushun, the climatic characters and causes of anomalous cold winter are analyzed. It is found that there is a cold period with the lowest temperature under -30℃ in the years of anomalous cold winter, as well as more snowfall and deep snow cover after global warming. By using the average ground temperature in deep level, sunspot activity, general circulation data, it can be found that the abnormal cold winter often occurs around the peak value year of macula activity, having a positive correlation with the average ground temperature at 0.8m below the surface during the prophase March-November, and the other properties are that the departure field of 500hPa geopotential height over Europe and Asia in northern hemisphere shows positive(negative) departure in west (east), the East Asia trough will establish steadily, and the general circulation appears as E pattern over Atlantic-Eurasia.
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吕志红,李强,李晶,侯波,王阳,王丽莉,2006.抚顺冬季异常偏冷年气候特征及成因分析[J].气象,32(9):90-94.
,2006.Analysis of Climatic Characteristics and Causes of Anomalous Cold Winter in Fushun, Liaoning[J].Meteor Mon,32(9):90-94.