The thermal state of permafrost under climate change on the Qinghai-Tibet Plateau (1980-2022) : A case study of the West Kunlun
The thermal regime is a key indicator of permafrost evolution and thaw trajectories in response to climate change but remains poorly represented in global models. In this study, we applied the Moving-Grid Permafrost Model (MGPM), an efficient numerical model, to simulate the permafrost thermal regime in West Kunlun (WKL), a 55 669 km2 region on the remote northwestern Qinghai-Tibet Plateau charact
