Articles | Volume 9, issue 1
https://doi.org/10.5194/tc-9-245-2015
https://doi.org/10.5194/tc-9-245-2015
Research article
 | 
09 Feb 2015
Research article |  | 09 Feb 2015

Heat sources within the Greenland Ice Sheet: dissipation, temperate paleo-firn and cryo-hydrologic warming

M. P. Lüthi, C. Ryser, L. C. Andrews, G. A. Catania, M. Funk, R. L. Hawley, M. J. Hoffman, and T. A. Neumann

Viewed

Total article views: 3,914 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,886 1,787 241 3,914 191 180
  • HTML: 1,886
  • PDF: 1,787
  • XML: 241
  • Total: 3,914
  • BibTeX: 191
  • EndNote: 180
Views and downloads (calculated since 13 Oct 2014)
Cumulative views and downloads (calculated since 13 Oct 2014)

Cited

Saved (final revised paper)

Saved (preprint)

Latest update: 25 Apr 2024
Download
Short summary
We analyze the thermal structure of the Greenland Ice Sheet with a heat flow model. New borehole measurements indicate that more heat is stored within the ice than would be expected from heat diffusion alone. We conclude that temperate paleo-firn and cyro-hydrologic warming are essential processes that explain the measurements.