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Changes in daily climate extremes in China and their connection to the large scale atmospheric circulation during 1961-2003 期刊论文
CLIMATE DYNAMICS, 2011, 卷号: 36, 期号: 11-12, 页码: 2399-2417
Authors:  You QL (游庆龙);  Kang SC (康世昌);  Aguilar E (Aguilar Enric);  Pepin N (Pepin Nick);  Flugel WA (Fluegel Wolfgang-Albert);  Yan YP (Yan Yuping);  Xu YW (徐彦伟);  Zhang YJ (张拥军);  Huang J (黄杰);  Kang, SC (通讯作者),Chinese Acad Sci CAS, Lab Tibetan Environm Changes & Land Surface Proc, Inst Tibetan Plateau Res, Beijing 100085, Peoples R China
Adobe PDF(1950Kb)  |  Favorite  |  View/Download：1712/325  |  Submit date：2012/05/10
TEMPERATURE EXTREMES  AIR-TEMPERATURE  TRENDS  URBANIZATION  RAINFALL  PRECIPITATION  VARIABILITY  REANALYSIS  PACIFIC  REGION  
Characteristics of extreme droughts inferred from tree-ring data in the Qilian Mountains, 1700-2005 期刊论文
CLIMATE RESEARCH, 2011, 卷号: 50, 期号: 2-3, 页码: 141-159
Authors:  Zhang Y (张勇);  Shao XM (邵雪梅);  Yin ZY (Yin Zhi-Yong);  Liang EY (梁尔源);  Tian QH (Tian Qinhua);  Xu Y (Xu Yan);  Shao XM (通讯作者),Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China
Adobe PDF(3452Kb)  |  Favorite  |  View/Download：1227/164  |  Submit date：2012/05/14
ASIAN SUMMER MONSOON  NORTHEASTERN TIBETAN PLATEAU  WESTERN NORTH PACIFIC  NORTHWESTERN CHINA  EASTERN CHINA  ATMOSPHERIC CIRCULATION  PRECIPITATION VARIATION  GENERAL-CIRCULATION  CLIMATE VARIABILITY  SEASONAL RAINFALL  
Observed changes in snow depth and number of snow days in the eastern and central Tibetan Plateau 期刊论文
CLIMATE RESEARCH, 2011, 卷号: 46, 期号: 2, 页码: 171-183
Authors:  You QL (游庆龙);  Kang SC (康世昌);  Ren GY (Ren Guoyu);  Fraedrich K (Fraedrich Klaus);  Pepin N (Pepin Nick);  Yan YP (Yan Yuping);  Ma, LJ (Ma Lijuan);  Kang SC (通讯作者),Chinese Acad Sci, Lab Tibetan Environm Changes & Land Surface Proc, Inst Tibetan Plateau Res, Beijing 100085, Peoples R China
Adobe PDF(1237Kb)  |  Favorite  |  View/Download：1314/106  |  Submit date：2012/05/14
NORTH-ATLANTIC OSCILLATION  MONSOON RAINFALL  SUMMER MONSOON  CLIMATE-CHANGE  COVER  VARIABILITY  TEMPERATURE  HEMISPHERE  WINTER  MODE