青藏高原热喀斯特湖演化及其对多年冻土的热影响模型计算研究
|
Study on numerical modeling of thermokarst lake evolution and its thermal impacts on permafrost on the Qinghai-Tibet Plateau
|
图4. 不同深度湖塘地下冰的初始状态 |
Fig. 4. Initial states of underground ice for the lake: 0.5 m deep (a), 1.0 m deep (b), 1.5 m deep (c) and 2.0 m deep (d) |
![]() |