Variation in the permafrost active layer over the Tibetan Plateau during 1980–2020OA
The active layer,acting as an intermediary of water and heat exchange between permafrost and atmosphere,greatly influences biogeochemical cycles in permafrost areas and is notably sensitive to climate fluctuations.Utilizing t…查看全部>>
Jinglong Huang;Chaofan Li;Binghao Jia;Chujie Gao;Ruichao Li
College of Oceanography,Hohai University,Nanjing,China Center for Monsoon System Research,Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing,ChinaCenter for Monsoon System Research,Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing,China College of Earth and Planetary Sciences,University of Chinese Academy of Sciences,Beijing,ChinaState Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics,Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing,ChinaCollege of Oceanography,Hohai University,Nanjing,ChinaState Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics,Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing,China
地质学
Active layer thicknessPermafrostTibetan plateauClimatological characteristics
《Atmospheric and Oceanic Science Letters》 2024 (5)
P.34-39,6
supported by the Second Tibetan Plateau Scientific Expedition and Research(STEP)program[grant number 2019QZKK0102]the Youth Innovation Promotion Association CAS[grant number 2021073]the special fund of the Yunnan University“double firstclass”construction.
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