Articles | Volume 12, issue 12
https://doi.org/10.5194/gmd-12-5291-2019
https://doi.org/10.5194/gmd-12-5291-2019
Model description paper
 | 
19 Dec 2019
Model description paper |  | 19 Dec 2019

Ground subsidence effects on simulating dynamic high-latitude surface inundation under permafrost thaw using CLM5

Altug Ekici, Hanna Lee, David M. Lawrence, Sean C. Swenson, and Catherine Prigent

Viewed

Total article views: 2,792 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,915 818 59 2,792 271 76 74
  • HTML: 1,915
  • PDF: 818
  • XML: 59
  • Total: 2,792
  • Supplement: 271
  • BibTeX: 76
  • EndNote: 74
Views and downloads (calculated since 02 May 2019)
Cumulative views and downloads (calculated since 02 May 2019)

Viewed (geographical distribution)

Total article views: 2,792 (including HTML, PDF, and XML) Thereof 2,491 with geography defined and 301 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 16 Jul 2024
Download
Short summary
Ice-rich permafrost thaw can create expanding thermokarst lakes as well as shrinking large wetlands. Such processes can have major biogeochemical implications and feedbacks to climate systems by altering the pathways and rates of permafrost carbon release. We developed a new model parameterization that allows a direct representation of surface water dynamics with subsidence. Our results show increased surface water fractions around western Siberian plains and northeastern territories of Canada.