青藏高原多年冻土区热融滑塌发育特征及规律
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The characteristics and patterns of retrogressive thaw slumps developed in permafrost region of the Qinghai-Tibet Plateau
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图5. 2008—2018年不同时期北麓河盆地热融滑塌数量和面积变化[修改自Luo等[ |
Fig.5. The number and area of thaw slumps interpreted from satellite images from 2008 to 2018 [revised from Luo et al[ |
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