基于GIS和RS的中亚阿拉套山脉近22年来冰川变化

[1] 近40年来冷龙岭地区冰川退缩和气候变化的关系 [J]. 水土保持研究, 2012, 19 (05) : 34 - 38

[2] 基于GIS的西藏林芝地区泥石流易发与危险区分析 [J]. 水土保持研究 , 2012, (03) : 195 - 199+301

[3] 近30年珠穆朗玛峰国家自然保护区冰川变化的遥感监测 [J]. 地理学报, 2010, 65 (01) : 13 - 28

[4] 川藏公路南线典型冰湖及其溃决危险性评价 [J]. 水土保持研究, 2009, 16 (02) : 50 - 55

[5] 希夏邦马峰东坡冰川与冰川湖泊变化遥感监测 [J]. 冰川冻土, 2005, (06) : 801 - 805

[6] 中国冰川系统变化趋势预测研究 [J]. 水土保持研究, 2005, (05) : 81 - 86

[7] Recent glacial retreat in High Asia in China and its impact on water resource in Northwest China[J]. YAO Tandong 1,2 ,WANG Youqing 2 ,LIU Shiying 2,1 ,PU Jianchen 2,1 ,SHEN Yongping 2 & LU Anxin 2,1 1.Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100029,China;2.Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences,Lanzhou 730000,China.Science in China(Series D:Earth Sciences). 2004(12)

[8] 近百年来青藏高原冰川的进退变化 [J]. 冰川冻土, 2004, (05) : 517 - 522

[9] Estimation on the response of glaciers in China to the global warming in the 21st century[J]. SHI Yafeng & LIU Shiyin Laboratory of Ice Core and Cold Regions Environment, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China;Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China.Chinese Science Bulletin. 2000(07)

[10] 青藏高原气候环境对冰川发育影响的数值模拟研究[D]. 王园香.中国气象科学研究院. 2009

[1] 近40年来冷龙岭地区冰川退缩和气候变化的关系 [J]. 水土保持研究, 2012, 19 (05) : 34 - 38

[2] 基于GIS的西藏林芝地区泥石流易发与危险区分析 [J]. 水土保持研究 , 2012, (03) : 195 - 199+301

[3] 近30年珠穆朗玛峰国家自然保护区冰川变化的遥感监测 [J]. 地理学报, 2010, 65 (01) : 13 - 28

[4] 川藏公路南线典型冰湖及其溃决危险性评价 [J]. 水土保持研究, 2009, 16 (02) : 50 - 55

[5] 希夏邦马峰东坡冰川与冰川湖泊变化遥感监测 [J]. 冰川冻土, 2005, (06) : 801 - 805

[6] 中国冰川系统变化趋势预测研究 [J]. 水土保持研究, 2005, (05) : 81 - 86

[7] Recent glacial retreat in High Asia in China and its impact on water resource in Northwest China[J]. YAO Tandong 1,2 ,WANG Youqing 2 ,LIU Shiying 2,1 ,PU Jianchen 2,1 ,SHEN Yongping 2 & LU Anxin 2,1 1.Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100029,China;2.Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences,Lanzhou 730000,China.Science in China(Series D:Earth Sciences). 2004(12)

[8] 近百年来青藏高原冰川的进退变化 [J]. 冰川冻土, 2004, (05) : 517 - 522

[9] Estimation on the response of glaciers in China to the global warming in the 21st century[J]. SHI Yafeng & LIU Shiyin Laboratory of Ice Core and Cold Regions Environment, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China;Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China.Chinese Science Bulletin. 2000(07)

[10] 青藏高原气候环境对冰川发育影响的数值模拟研究[D]. 王园香.中国气象科学研究院. 2009