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Glacier change in the Gangdise Mountains, southern Tibet, since the Little Ice Age 期刊论文
GEOMORPHOLOGY, 2018, 卷号: 306, 期号: 0, 页码: 51-63
Authors:  Zhang, Q (Zhang, Qian);  Yi, CL (Yi, Chaolu);  Fu, P (Fu, Ping);  Wu, YB (Wu, Yubin);  Liu, JH (Liu, Jinhua);  Wang, NL (Wang, Ninglian)
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Be-10 Surface Exposure  Climate-change  Tian-shan  Plateau  Uplift  Area  Temperature  Millennium  Asymmetry  Inventory  
Geomorphology of anomalously high glaciated mountains at the northwestern end of Tibet: Muztag Ata and Kongur Shan 期刊论文
GEOMORPHOLOGY, 2009, 卷号: 103, 期号: 2, 页码: 227-250 Sp
Authors:  Seong;  YB (Seong;  Yeong Bae);  Owen;  LA (Owen;  Lewis A.);  YI CL(易潮路);  Finkel;  RC (Finkel;  Robert C.);  Schoenbohm;  L (Schoenbohm;  Lindsay)
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Equilibrium-line Altitudes  Nanga Parbat Himalaya  Cosmogenic Nuclides  Erosion Rates  Sediment Production  Landscape Response  Garhwal Himalaya  Denudation Rates  River Sediments  Northern India  
Integrated research on mountain glaciers: Current status, priorities and future prospects 期刊论文
GEOMORPHOLOGY, 2009, 卷号: 103, 期号: 2, 页码: 158-171
Authors:  Owen;  LA (Owen;  Lewis A.);  Thackray;  G (Thackray;  Glenn);  Anderson;  RS (Anderson;  Robert S.);  Briner;  J (Briner;  Jason);  Kaufman;  D (Kaufman;  Darrell);  Roe;  G (Roe;  Gerard);  Pfeffer;  W (Pfeffer;  William);  Yi CL(易潮路)
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Late Quaternary Glaciation  Lake Outburst Floods  Ice Core Evidence  Climate-change  Sea-level  Polythermal Glacier  Tibetan Plateau  Sierra-nevada  Mass-balance  Erosion  
Relationships between the heights of moraines and lengths of former glaciers in Tibet and surrounding mountains 期刊论文
GEOMORPHOLOGY, 2009, 卷号: 103, 期号: 2, 页码: 205-211 Sp
Authors:  Fu P(傅平);  Yi CL(易潮路)
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Ice-sheet  Glaciation  Plateau  Landforms  Himalaya  Valley  Extent  Andes  
Mountain glaciation and landscape evolution 期刊论文
GEOMORPHOLOGY, 2009, 卷号: 103, 期号: 2, 页码: 155-157
Authors:  Owen;  LA (Owen;  Lewis A.);  Thackray;  G (Thackray;  Glenn);  Yi CL(易潮路)
Adobe PDF(125Kb)  |  Favorite  |  View/Download:896/123  |  Submit date:2010/04/30
Erosion  Climate  Ranges  Limits  Uplift  Rates