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我国东西部地区地气温差的年代际变化特征
引用本文:温李明,周连童,黄荣辉,范广洲.我国东西部地区地气温差的年代际变化特征[J].气候与环境研究,2014,19(5):636-648.
作者姓名:温李明  周连童  黄荣辉  范广洲
作者单位:成都信息工程学院, 成都 610225;中国科学院大气物理研究所季风系统研究中心, 北京 100190;中国科学院大气物理研究所季风系统研究中心, 北京 100190;中国科学院大气物理研究所季风系统研究中心, 北京 100190;成都信息工程学院, 成都 610225
基金项目:国家自然科学基金项目41175055、41230527
摘    要:利用1960~2006年我国地温、气温逐日4个时次02:00(北京时间,下同)、08:00、14:00和20:00]的台站观测资料,计算并分析了我国东南、西北地区各季地气温差的年代际变化特征。分析结果表明:我国东南部地区各季地气温差在20世纪70年代末以前,大部分年份偏高,高于平均值,而在20世纪70年代末以后,我国东南部地区各季地气温差偏低,在夏季和冬季表现尤为明显。我国西北地区春季和夏季地气温差在20世纪70年代末以前大部分年份偏低,低于平均值;而在20世纪70年代末以后,地气温差则大部分年份明显偏高。我国西北地区秋季地气温差的年代际变化特征不明显,而冬季地气温差的年代际变化趋势与春夏季相反,在20世纪70年代末以前大部分年份偏高,高于平均值,而在20世纪70年代末以后偏低。另外,发现地温和气温对我国东南、西北地区各季地气温差的年代际变化在各季所起的贡献作用不同。

关 键 词:东西部地区  地气温差  年代际变化
收稿时间:2013/6/14 0:00:00
修稿时间:9/6/2013 12:00:00 AM

Characteristics of Interdecadal Variability in the Difference Between Surface Temperature and Surface Air Temperature in Southeast and Northwest China
WEN Liming,ZHOU Liantong,HUANG Ronghui and FAN Guangzhou.Characteristics of Interdecadal Variability in the Difference Between Surface Temperature and Surface Air Temperature in Southeast and Northwest China[J].Climatic and Environmental Research,2014,19(5):636-648.
Authors:WEN Liming  ZHOU Liantong  HUANG Ronghui and FAN Guangzhou
Institution:Chengdu University of Information Techology, Chegndu 610225;Center for Monsoon System Research, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100190;Center for Monsoon System Research, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100190;Center for Monsoon System Research, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100190;Chengdu University of Information Techology, Chegndu 610225
Abstract:The characteristics of the interdecadal variability in the differences between surface temperature (Ts) and surface air temperature (Ta) are analyzed, using daily-observed surface temperature and surface air temperature data from 1960 to 2006. Analysis results show that there is a clear interdecadal variability in Ts-Ta in Southeast and Northwest China. Before the late 1970s, the Ts-Ta anomalies were mostly positive in Southeast China, but they mostly became negative after this period. In contrast, in Northwest China, the Ts-Ta anomalies were mostly negative in spring and summer before the late 1970s, but became largely positive after this time. The opposite trend can be seen in the variability of Ts-Ta in Northwest China in the winter. However, in the autumn in Northwest China, the interdecadal variability of Ts-Ta was not as clear as during the other seasons. The analyzed results of Ts and Ta over the study period show that their contributions to interdecadal variability of in Ts-Ta differed between different seasons.
Keywords:Southeast China and Northwest China  Ts-Ta  Interdecadal variability
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