摘要
Global warming is causing the Tibetan permafrost to degrade, as evidenced by rising ground temperatures, thicker active layer thickness, thinner permafrost layer, and melting underground ice, etc.(Ran et al., 2018;Wang et al., 2020).The degradation of permafrost not only profoundly alters the carbon cycling processes in high-altitude ecosystems,thereby influencing the regional climate system, but also affects landscape hydrological connectivity。
基金
supported by the Second Tibetan Plateau Scientific Expedition and Research Program (Grant No. 2022QZKK0101)
the West Light Foundation of the Chinese Academy of Sciences (Grant No. xbzg-zdsys-202202)
the Science and Technology Major Project of Xizang Autonomous Region of China (XZ202201ZD0005G04)。