Articles | Volume 12, issue 10
https://doi.org/10.5194/tc-12-3215-2018
https://doi.org/10.5194/tc-12-3215-2018
Research article
 | 
08 Oct 2018
Research article |  | 08 Oct 2018

Processes influencing heat transfer in the near-surface ice of Greenland's ablation zone

Benjamin H. Hills, Joel T. Harper, Toby W. Meierbachtol, Jesse V. Johnson, Neil F. Humphrey, and Patrick J. Wright

Viewed

Total article views: 2,607 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,528 1,008 71 2,607 328 58 48
  • HTML: 1,528
  • PDF: 1,008
  • XML: 71
  • Total: 2,607
  • Supplement: 328
  • BibTeX: 58
  • EndNote: 48
Views and downloads (calculated since 02 May 2018)
Cumulative views and downloads (calculated since 02 May 2018)

Viewed (geographical distribution)

Total article views: 2,607 (including HTML, PDF, and XML) Thereof 2,347 with geography defined and 260 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (final revised paper)

Latest update: 19 Apr 2024
Download
Short summary
At its surface, an ice sheet is closely connected to the climate. Assessing heat transfer between near-surface ice and the overlying atmosphere is important for understanding how the ice sheet is melting at the surface. We measured ice temperature within 20 m of the surface of the Greenland Ice Sheet. Resulting ice temperatures are warmer than the air, a peculiar result which implies the role of some nonconductive heat transfer processes such as latent heating by refreezing meltwater.