Articles | Volume 11, issue 6
https://doi.org/10.5194/tc-11-2799-2017
https://doi.org/10.5194/tc-11-2799-2017
Research article
 | 
11 Dec 2017
Research article |  | 11 Dec 2017

A continuum model for meltwater flow through compacting snow

Colin R. Meyer and Ian J. Hewitt

Viewed

Total article views: 4,104 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,047 1,914 143 4,104 672 130 125
  • HTML: 2,047
  • PDF: 1,914
  • XML: 143
  • Total: 4,104
  • Supplement: 672
  • BibTeX: 130
  • EndNote: 125
Views and downloads (calculated since 19 Jul 2017)
Cumulative views and downloads (calculated since 19 Jul 2017)

Viewed (geographical distribution)

Total article views: 4,104 (including HTML, PDF, and XML) Thereof 3,808 with geography defined and 296 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 22 Nov 2024
Download
Short summary
We describe a new model for the evolution of snow temperature, density, and water content on the surface of glaciers and ice sheets. The model encompasses the surface hydrology of accumulation and ablation areas, allowing us to explore the transition from one to the other as thermal forcing varies. We predict year-round liquid water storage for intermediate values of the surface forcing. We also compare our model to data for the vertical percolation of meltwater in Greenland.