机译:青藏高原东部黄河源区与地貌相关的多年冻土特征
Lanzhou Univ, Cold & Arid Reg Environm & Engn Res Inst, State Key Lab Frozen Soil Engn, Lanzhou 730000, Peoples R China|Michigan State Univ, Dept Geog Environm & Spatial Sci, E Lansing, MI 48224 USA;
Lanzhou Univ, Cold & Arid Reg Environm & Engn Res Inst, State Key Lab Frozen Soil Engn, Lanzhou 730000, Peoples R China;
Lanzhou Univ, Cold & Arid Reg Environm & Engn Res Inst, State Key Lab Frozen Soil Engn, Lanzhou 730000, Peoples R China;
Lanzhou Univ, Cold & Arid Reg Environm & Engn Res Inst, State Key Lab Frozen Soil Engn, Lanzhou 730000, Peoples R China;
Lanzhou Univ, Cold & Arid Reg Environm & Engn Res Inst, State Key Lab Frozen Soil Engn, Lanzhou 730000, Peoples R China|Gansu Inst Civil Engn, Lanzhou 73000, Peoples R China;
Lanzhou Univ, Cold & Arid Reg Environm & Engn Res Inst, State Key Lab Frozen Soil Engn, Lanzhou 730000, Peoples R China;
Shanxi Reg Elect Power Design Co Ltd, Xian 710000, Peoples R China;
China; Ground temperature; Permafrost; Landforms; Yellow River;
机译:青藏高原黄河源区多年冻土退化对径流的影响
机译:中国青藏高原黄河源区降解永久冻土对流的影响
机译:青藏高原长江黄河源区暖干多年冻土的热力与地表温度的关系
机译:中国东北地区黄河源区多年冻土的分布
机译:中国青藏高原高原多年冻土的某些方面,以及与加拿大麦肯齐三角洲地区的比较