The Cryosphere
The Cryosphere
TC
Articles | Volume 20, issue 5
Articles | Volume 20, issue 5
https://doi.org/10.5194/tc-20-2681-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-20-2681-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 20, issue 5
Research article
 | 
08 May 2026
Research article |  | 08 May 2026

Ensemble numerical simulation of permafrost thermal regimes over the Tibetan Plateau using the Flexible Permafrost Model: 1950–2023

Wen Sun and Bin Cao

Viewed

Total article views: 8,355 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
6,740 1,349 266 8,355 234 208 327
  • HTML: 6,740
  • PDF: 1,349
  • XML: 266
  • Total: 8,355
  • Supplement: 234
  • BibTeX: 208
  • EndNote: 327
Views and downloads (calculated since 25 Jun 2025)
Cumulative views and downloads (calculated since 25 Jun 2025)

Viewed (geographical distribution)

Total article views: 8,355 (including HTML, PDF, and XML) Thereof 8,310 with geography defined and 45 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 08 May 2026
Download
Short summary
Understanding the dynamics of permafrost heavily relies on process-based simulations. In this study, we introduce a new model specifically designed for permafrost applications, the Flexible Permafrost Model (FPM). This model serves as an adaptable framework for implementing innovative permafrost-related physics. Long-term ensemble simulations indicate that the permafrost temperature increased at a rate of 0.11 °C dec-1 since 1980 with a decreased area of ∼12.4 % over the Tibetan Plateau.
Read more
Share