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青藏高原不同季节地表温度变化特征分析
引用本文:何冬燕,田红,邓伟涛.青藏高原不同季节地表温度变化特征分析[J].南京信息工程大学学报,2014(6):558-569.
作者姓名:何冬燕  田红  邓伟涛
作者单位:1. 安徽省气候中心,合肥,230031
2. 南京信息工程大学 气象灾害省部共建教育部重点实验室,南京,210044
基金项目:安徽省自然科学基金(090415216);江苏省高校自然科学研究面上项目(10KJB170007);国家自然科学基金青年基金
摘    要:基于欧洲中尺度气象预报中心(ECMWF)提供的ERA-Interim地表温度,利用经验正交函数(EOF)等方法,分析了青藏高原四季地表温度的时空变化特征.结果发现:青藏高原春、夏、冬季地表温度变化以整体型为主,并且大部地区地表温度呈现升高的趋势;秋季地表温度略有下降趋势,并且以东部和西部地表温度的反向型异常变化最为显著.此外还发现,青藏高原不同季节地表温度的异常变化具有一定的联系,其中整体型变化可以持续3个季节.

关 键 词:青藏高原  地表温度  经验正交函数  异常变化

Characteristics of seasonal surface temperature variation over the Tibetan Plateau
HE Dongyan,TIAN Hong,DENG Weitao.Characteristics of seasonal surface temperature variation over the Tibetan Plateau[J].Journal of Nanjing University of Information Science & Technology,2014(6):558-569.
Authors:HE Dongyan  TIAN Hong  DENG Weitao
Affiliation:HE Dongyan, TIAN Hong, DENG Weitao ( 1 Anhui Climate Center,Hefei 230031 2 Key Laboratory of Meteorological Disaster of Ministry of Education, Nanjing University of Information Science & Technology, Nanjing 210044)
Abstract:The ERA-Interim surface temperature data from European Centre for Medium Range Weather Forecasts ( ECMWF) are used to analyze the spatial and temporal variation of the seasonal surface temperature over the Tibet-an Plateau using Empirical Orthogonal Function(EOF).The results show that in spring,summer and winter,the sur-face temperature tends to increase in the whole Plateau without obvious spatial variation;while in autumn,surface temperature tends to decrease slightly in most area,and a significant opposite variation trend exists between the east-ern and western area of the Plateau. In addition,there are some definite relations between the surface temperature anomaly variations in different seasons,and the integral type can last for 3 seasons.
Keywords:the Tibetan Plateau  the surface temperature  Empirical Orthogonal Function(EOF)  anomaly variations
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