【作者】Hu Li，Xiaoduo Pan，Xiaoqing Peng，Rana Muhammad Ali Washakh，Min Zheng，Xiaowei Nie
【作者单位】1National Tibetan Plateau Data Center (TPDC), State Key Laboratory of Tibetan Plateau Earth System, Environment and Resources (TPESER), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China;2University of the Chinese Academy of Sciences, Beijing 100049, China;3Academy of Plateau Science and Sustainability, Qinghai Normal University, Xining 810016, China;4Key Laboratory of Western China's Environmental Systems, Ministry of Education, College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China;5School of Civil Engineering, Guizhou Institute of Technology, Guiyang 550003, China;6School of Ecology and Environment, Tibet University, Lhasa 850000, China
【摘要】 In the context of global warming, the soil freeze depth over the Tibetan Plateau has undergone significant changes, with a series of profound impacts on the hydrological cycle and ecosystem. The complex terrains and high elevations of the TP pose g...
