Articles | Volume 14, issue 9
https://doi.org/10.5194/tc-14-3155-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-14-3155-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Evaluating permafrost physics in the Coupled Model Intercomparison Project 6 (CMIP6) models and their sensitivity to climate change
Eleanor J. Burke
CORRESPONDING AUTHOR
Met Office Hadley Centre, FitzRoy Road, Exeter, EX1 3PB, UK
Canada Centre for Mapping and Earth Observation, Natural Resources Canada, Ottawa, Ontario, Canada
Gerhard Krinner
Institut des Géosciences de l'Environnement, CNRS, Université Grenoble Alpes, Grenoble, France
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- Characterizing the Changes in Permafrost Thickness across Tibetan Plateau Y. Zhao et al. 10.3390/rs15010206
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Latest update: 07 Dec 2023
Short summary
Permafrost will degrade under future climate change. This will have implications locally for the northern high-latitude regions and may well also amplify global climate change. There have been some recent improvements in the ability of earth system models to simulate the permafrost physical state, but further model developments are required. Models project the thawed volume of soil in the top 2 m of permafrost will increase by 10 %–40 % °C−1 of global mean surface air temperature increase.
Permafrost will degrade under future climate change. This will have implications locally for the...