Articles | Volume 9, issue 5
https://doi.org/10.5194/tc-9-1845-2015
https://doi.org/10.5194/tc-9-1845-2015
Research article
 | 
22 Sep 2015
Research article |  | 22 Sep 2015

Ice sheet mass loss caused by dust and black carbon accumulation

T. Goelles, C. E. Bøggild, and R. Greve

Viewed

Total article views: 4,434 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,050 2,218 166 4,434 404 142 138
  • HTML: 2,050
  • PDF: 2,218
  • XML: 166
  • Total: 4,434
  • Supplement: 404
  • BibTeX: 142
  • EndNote: 138
Views and downloads (calculated since 23 Apr 2015)
Cumulative views and downloads (calculated since 23 Apr 2015)

Cited

Saved (final revised paper)

Saved (preprint)

Latest update: 27 Mar 2024
Download
Short summary
Soot (black carbon) and dust particles darken the surface of ice sheets and glaciers as they accumulate. This causes more ice to melt, which releases more particles from within the ice. This positive feedback mechanism is studied with a new two-dimensional model, mimicking the conditions of Greenland, under different climate warming scenarios. In the warmest scenario, the additional ice sheet mass loss until the year 3000 is up to 7%.