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SHI Ya feng 1, SHEN Yong ping 1, HU Ru ji 2(1.Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Science, Lanzhou Gansu 730000, China; 2. Xinjiang Institute of Ecology and Geography, Chinese Academy of Scie;Preliminary Study on Signal, Impact and Foreground of Climatic Shift from Warm-Dry to Warm-Humid in Northwest China[J];Journal of Glaciolgy and Geocryology;2002-03 |
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ZHANG Dong-qi~{1, 2}, QIN Da-he~{1, 2}, HOU Shu-gui~2,KANG Shi-chang~{2, 3}, REN Jia-wen~2 ratory of Ice Core andCold Regions Environment, CAREERI, CAS, Lanzhou Gansu 730000, China; 3. Institute for Quaternaryand Climate Studies, University of Maine, Orono Maine, USA);Net Accumulation Rate of the East Rongbuk Glacierand Indian Summer Monsoon Rainfall[J];Journal of Glaciology and Geocryology;2004-02 |
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LU Ai-gang~1, GE Jian-ping~2, PANG De-qian~1, HE Yuan-qing~3, PANG Hong-xi~3 (1.Institute of Geography Research,Weinan Teachers College,Weinan Shaanxi 714000,China;2.Ministry ofEducation Key Laboratory for Biodiversity Science and Engineering,College of Life Sciences,Beijing NormalUniversity,Beijing 100875,China;3.Cold and Arid Regions Environmental and Engineering Institute,Chinese Academy of Sciences,Lanzhou Gansu 730000,China);Asynchronous Response of Droughts to ENSO in China[J];Journal of Glaciology and Geocryology;2006-04 |
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LAN Yong-chao~1,2, SHEN Yong-ping~1, LIN Shu~3, ZHANG Shi-qian~1, CHANG Jun-jie~2,(1.Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Acadeny of Sciences,Lanzhou Gansu 730000,China;2.Institute of the Yellow River Riverhead,Water Conservancy Committee in the Yellow River Basin,Lanzhou Gansu 730000,China3.Lanzhou Central Meteorological Observatory,Lanzhou Gansu 730020,China;);Changes in High and Low Flow Cycles of the Upper Reaches of Yellow River and Their Circumfluence Backdrop[J];Journal of Glaciology and Geocryology;2006-06 |
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GENG Zhi-xin1,2,HOU Shu-gui1,ZHANG Dong-qi1,3,KANG Shi-chang1,4,SUN Xi-mei2(1.State Key Laboratory of Cryospheric Science,AREERI,CAS,Lanzhou Gansu 730000,China;2.Huantai No.1 Middle School,Zibo Shandong 256400,China;3.Chinese Academy of Meteorological Sciences,Beijing 100081,China;4.Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100085,China);A High-Resolution Ice Core Record from Mount Qomolangma since 1844 AD[J];Journal of Glaciology and Geocryology;2007-05 |
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XIN Guojun (Department of Geophysics, Beijing University, Beijing, 100871);Hierarchical Structure of SAT Variations and Trend of Future Climate Change[J];ACTA SCICENTIARUM NATURALUM UNIVERSITIS PEKINESIS;1997-02 |
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SONG Yan~(1,2);JI Jin-jun~2;ZHU Lin-hong~3;ZHANG Shi-ying~3.1 China Meteorological Administration Training Centre,Beijing,100081,P.R.China;2 Key Laboratory of Regional Climate-Environment Research for Temperate East Asia,Chinese Academy of Sciences,Beijing,100029,P.R.China;3 Shanxi Meteorological Administration,Taiyuan,030002,P.R.China.;Characteristics of Asian-African summer monsoon pre-and post-global warming in mid-1980s.[J];Journal of Beijing Forestry University;2007-02 |
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Pan Yaozhong;Gong Daoyi;Wang Ping (Department of Resources and Environmental Sciences , Beijing Normal University; Environmental Changes and Natural Disaster Open Research Laboratory, National Education Commision; 100875, Beijing, PRC);A RESEARCH ON TEMPORAL-SPATIAL CHARACTERISTICS OF DROUGHT IN CHINA DURING 1949 ~1990[J];JOURNAL OF BEIJING NORMAL UNIVERSITY;1996-01 |
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Li Chao (Research Department of Chengdu Institute of Meteorology);THE TYPICAL STRUCTURE,THE ANNUAL VARIATION AND THE CLIMATIC JUMP O'F THE PRECIPITAION IN FLOOD SEASONS IN CHINA[J];;1990-04 |
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LIN Xuedong1,2, ZHANG Yili2, YAO Zhijun2, GONG Tongliang3,4, WANG Hong5, LIU Linshan2 (1. Institute of Tibetan Plateau Research, CAS, Beijing 100085, China; 2. Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing 100101, China; 3. Tibet Hydroelectric Investigation, Designed Research Institute, Lhasa 850000, China; 4. School of Civil Engineering, Tsinghua University, Beijing, 100084, China; 5. Tibet Hydrographic and Water Resources Survey Bureau, Lhasa 850000, China);Trend Analysis of the Runoff Variation in Lhasa River Basin in Tibetan Plateau during the Last 50 Years[J];Progress in Geography;2007-03 |
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