Articles | Volume 14, issue 9
https://doi.org/10.5194/tc-14-3155-2020
https://doi.org/10.5194/tc-14-3155-2020
Research article
 | 
16 Sep 2020
Research article |  | 16 Sep 2020

Evaluating permafrost physics in the Coupled Model Intercomparison Project 6 (CMIP6) models and their sensitivity to climate change

Eleanor J. Burke, Yu Zhang, and Gerhard Krinner

Viewed

Total article views: 9,058 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
6,644 2,283 131 9,058 526 113 153
  • HTML: 6,644
  • PDF: 2,283
  • XML: 131
  • Total: 9,058
  • Supplement: 526
  • BibTeX: 113
  • EndNote: 153
Views and downloads (calculated since 07 Feb 2020)
Cumulative views and downloads (calculated since 07 Feb 2020)

Viewed (geographical distribution)

Total article views: 9,058 (including HTML, PDF, and XML) Thereof 8,338 with geography defined and 720 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 20 Nov 2024
Download
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.