Response of peat-rich permafrost to a warming climate on the northeast Tibetan Plateau

Author:

Du RanORCID,Peng Xiaoqing,Wang Kang,Frauenfeld Oliver W.,Chen CongORCID,Sun Wen,Jin Haodong,Zhao Yaohua,Peng SijiaORCID,Liang Benben

Funder

Fundamental Research Funds for the Central Universities

Lanzhou University

National Natural Science Foundation of China

State Key Laboratory of Frozen Soil Engineering

Qinghai Provincial Department of Science and Technology

Publisher

Elsevier BV

Subject

Atmospheric Science,Agronomy and Crop Science,Global and Planetary Change,Forestry

Reference63 articles.

1. Mathematical Modeling of Melting and Freezing Processes;Alexiades,1992

2. Global warming and active-layer thickness: results from transient general circulation models;Anisimov;Glob. Planet. Chang,,1997

3. Influences and interactions of inundation, peat, and snow on active layer thickness;Atchley;Geophys. Res. Lett.,2016

4. Permafrost is warming at a global scale;Biskaborn;Nat. Commun.,2019

5. Permafrost thaw accelerates in boreal peatlands during late-20th century climate warming;Camill;Clim. Chang.,2005

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