Articles | Volume 11, issue 7
https://doi.org/10.5194/gmd-11-2955-2018
https://doi.org/10.5194/gmd-11-2955-2018
Model description paper
 | 
24 Jul 2018
Model description paper |  | 24 Jul 2018

SHAKTI: Subglacial Hydrology and Kinetic, Transient Interactions v1.0

Aleah Sommers, Harihar Rajaram, and Mathieu Morlighem

Viewed

Total article views: 2,805 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,796 959 50 2,805 186 86 73
  • HTML: 1,796
  • PDF: 959
  • XML: 50
  • Total: 2,805
  • Supplement: 186
  • BibTeX: 86
  • EndNote: 73
Views and downloads (calculated since 27 Mar 2018)
Cumulative views and downloads (calculated since 27 Mar 2018)

Viewed (geographical distribution)

Total article views: 2,805 (including HTML, PDF, and XML) Thereof 2,581 with geography defined and 224 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 26 Apr 2024
Download
Short summary
Meltwater drainage beneath glaciers and ice sheets influences how fast they move and is complicated and constantly changing. Most models distinguish between fast and slow drainage with different equations for each system. The SHAKTI model allows for the ice–water drainage arrangement to transition naturally between different types of flow. This model can be used to understand how drainage affects glacier speeds and the associated ice loss to further inform predictions of sea level rise.