冻土生态环境团队
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代表性成果

代表性成果(10篇)

(1)Mu C, Abbott BW, Norris AJ,et al. The status and stability of permafrost carbon on the Tibetan Plateau.Earth-Science Reviews, 2020, 211, 103433.

(2)Mu C, Mu M, Wu X, et al. (2023). High carbon emissions from thermokarst lakes and their determinants in the Tibet Plateau, Global Change Biology, 29(10), 2732-2745.

(3)Mu C, Zhang F, Chen X,et al. Carbon and mercury export from the Arctic rivers and response to permafrost degradation.Water Research, 2019, 161, 54-60.

(4)Peng X, Zhang T, Frauenfeld OW, et al. (2023). Active Layer Thickness and Permafrost Area Projections for the 21st Century, Earth's Future, 11(8), e2023EF003573.

(5)Peng X, Zhang T, Frauenfeld OW,et al. Spatiotemporal changes in active layer thickness under contemporary and projected climate in the Northern Hemisphere,Journal of Climate, 2018, 31(1), 251-266.

(6)Peng X, Zhang T, Frauenfeld OW,et al. Response of seasonal soil freeze depth to climate change across China,The Cryosphere, 2017, 11, 1059-1073.

(7)Lu X, Gu W, Zhao L,et al. Methylmercury uptake and degradation by methanotrophs.Science Advances, 2017, 3(5), e1700041.

(8)Zhang G, Nan Z, Hu N, et al. Qinghai‐Tibet Plateau permafrost at risk in the late 21st century,Earth's Future, 2022, 10(6), e2022EF002652.

(9)Zhang G, Nan Z, Zhao L, et al. Qinghai-Tibet Plateau wetting reduces permafrost thermal responses to climate warming,Earth and Planetary Science Letters, 2021, 562, 116858.

(10)Zhang G, Nan Z, Wu X, et al. The role of winter warming in permafrost change over the Qinghai‐Tibet Plateau,Geophysical Research Letters, 2019, 46(20), 11261-11269.