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平流层各层温度变化的时空特征分析
引用本文:陈权亮,刘晓冉,李国平.平流层各层温度变化的时空特征分析[J].中国科学技术大学学报,2008,38(1):57-63.
作者姓名:陈权亮  刘晓冉  李国平
作者单位:1. 成都信息工程学院高原大气与环境四川高校重点实验室,成都,610225
2. 成都信息工程学院高原大气与环境四川高校重点实验室,成都,610225;重庆市气候中心,重庆,401147
基金项目:中国科学院大气物理研究所"联合创新青年学者计划" , 成都信息工程学院引进人才科研启动项目
摘    要:利用欧洲中心的ECMWF月平均温度场再分析资料分析了平流层各个层次温度变化的空间分布特征,结果表明1958-2001年全球平流层不同高度温度的变化有一定的差异.在平流层上层2hPa,温度呈显著的下降趋势;平流层中层20hPa温度场低纬度地区和高纬度地区相反变化,低纬度地区呈显著的下降;平流层下层70hPa温度场除了南半球高纬度地区外也呈下降趋势.同时,分析了不同区域温度变化的趋势和周期特征,平流层不同层次温度变化周期有着一定的差异,温度下降区域和温度上升区域的突变时间也有着明显的不同.

关 键 词:平流层  温度变化  经验正交函数(EOF)  小波分析  平流层  温度变化  时空特征分析  stratosphere  temperature  variations  突变时间  温度上升  温度下降  变化周期  周期特征  区域  南半球  高纬度地区  低纬度  平均温度场  中层  趋势  差异  不同高度  结果
文章编号:0253-2778(2008)01-0057-07
收稿时间:2007-08-10
修稿时间:2007-11-08

Space-time feature analysis of temperature variations in the stratosphere
CHEN Quan-liang,LIU Xiao-ran,LI Guo-ping.Space-time feature analysis of temperature variations in the stratosphere[J].Journal of University of Science and Technology of China,2008,38(1):57-63.
Authors:CHEN Quan-liang  LIU Xiao-ran  LI Guo-ping
Abstract:The spatial distribution characteristics of temperature variations in each stratospheric layer was analyzed through using monthly average temperature data of ECMWF reanalysis. The research result shows that, from 1958 to 2001, the temperature in the higher stratosphere about 2 hPa level decreased remarkably in the whole global; and in the middle stratosphere about 20 hPa level, the temperature in low latitude areas changed opposite to that in high latitude areas and the temperature in low latitude areas decreased evidently; at the same time, the temperature in the lower stratosphere about 70 hPa level showed a decreasing trend except over the high latitude areas of South Hemisphere. Meanwhile, Morlet wavelet analysis was used to analyze the trend and the periodicity of temperature variations in different regions in the stratosphere. The analysis results show that the temperatures in different levels have different periods, and the times of abrupt temperature changes in the temperature-down region are also evidently different from the temperature-up region.
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