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近50 a平流层强爆发性增温事件及其变化规律分析
引用本文:盛日锋,王盘兴,闵凡花.近50 a平流层强爆发性增温事件及其变化规律分析[J].南京气象学院学报,2005,28(2):241-247.
作者姓名:盛日锋  王盘兴  闵凡花
作者单位:南京信息工程大学,大气科学系,江苏,南京,210044
基金项目:国家自然科学基金重点资助项目(402333037)
摘    要:按WMO提供的标准,提出了划分强爆发性增温(Sudden Stratospheric Warming,简称SSW)事件的指标,用NCEP/NCAR 30 hPa层逐日温度、高度资料,确定了1950-2002年1-3月期间的35次强SSW事件。在此基础上,给出了强SSW事件发生的气候及异常特征,并从北半球中高纬臭氧及日照年际变化及其年际异常出发,给出了这些特征的部分成因。

关 键 词:平流层  强爆发性增温  大气臭氧
文章编号:1000-2022(2005)02-0241-07

Analysis of Strong SSW Events and Its Variation Rule in the Past Fifty Years
SHENG Ri-feng,WANG Pan-xing,MIN Fan-hua.Analysis of Strong SSW Events and Its Variation Rule in the Past Fifty Years[J].Journal of Nanjing Institute of Meteorology,2005,28(2):241-247.
Authors:SHENG Ri-feng  WANG Pan-xing  MIN Fan-hua
Abstract:Two indices for strong SSW events are put forward in this paper,according to the WMO standards.Using the NCEP/NCAR reananysis daily temperature and height data at 30hPa level,35 strong SSW events during January to March from 1950 to 2002 are determined.The climate and its anomalous features of SSW events are given,and their formation mechanism is partly explained by the interannual change and abnormality of sunshine and ozone distribution in the mid-high latitudes in the Northern Hemisphere.
Keywords:stratosphere  strong Sudden Stratospheric Warming  atmospheric ozone
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