Journal cover Journal topic
The Cryosphere An interactive open-access journal of the European Geosciences Union
Journal topic

Journal metrics

Journal metrics

  • IF value: 4.790 IF 4.790
  • IF 5-year value: 5.921 IF 5-year
    5.921
  • CiteScore value: 5.27 CiteScore
    5.27
  • SNIP value: 1.551 SNIP 1.551
  • IPP value: 5.08 IPP 5.08
  • SJR value: 3.016 SJR 3.016
  • Scimago H <br class='hide-on-tablet hide-on-mobile'>index value: 63 Scimago H
    index 63
  • h5-index value: 51 h5-index 51
Volume 9, issue 5
The Cryosphere, 9, 1845–1856, 2015
https://doi.org/10.5194/tc-9-1845-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: Interactions between climate change and the Cryosphere: SVALI,...

The Cryosphere, 9, 1845–1856, 2015
https://doi.org/10.5194/tc-9-1845-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 22 Sep 2015

Research article | 22 Sep 2015

Ice sheet mass loss caused by dust and black carbon accumulation

T. Goelles et al.
Download
Interactive discussion
Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement
Peer review completion
AR: Author's response | RR: Referee report | ED: Editor decision
AR by Thomas Goelles on behalf of the Authors (17 Jul 2015)  Author's response
ED: Publish subject to minor revisions (Editor review) (07 Aug 2015) by Jonathan Bamber
AR by Thomas Goelles on behalf of the Authors (18 Aug 2015)  Author's response    Manuscript
ED: Publish as is (24 Aug 2015) by Jonathan Bamber
Publications Copernicus
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%.
Soot (black carbon) and dust particles darken the surface of ice sheets and glaciers as they...
Citation