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
TC | Volume 12, issue 3
The Cryosphere, 12, 971–991, 2018
https://doi.org/10.5194/tc-12-971-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
The Cryosphere, 12, 971–991, 2018
https://doi.org/10.5194/tc-12-971-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 22 Mar 2018

Research article | 22 Mar 2018

Modelling seasonal meltwater forcing of the velocity of land-terminating margins of the Greenland Ice Sheet

Conrad P. Koziol and Neil Arnold
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 Conrad Koziol on behalf of the Authors (25 Jan 2018)  Author's response    Manuscript
ED: Publish subject to technical corrections (09 Feb 2018) by Andreas Vieli
AR by Conrad Koziol on behalf of the Authors (13 Feb 2018)  Author's response    Manuscript
Publications Copernicus
Download
Short summary
We model the summer acceleration of ice velocities at a land-terminating margin of the Greenland Ice Sheet. Model results compare favourably against GPS data, reflecting positively on the model components and the datasets used. When we run the model into the future, we find that summer velocities increase with increasing levels of surface melt but that changes in annual velocities may be limited.
We model the summer acceleration of ice velocities at a land-terminating margin of the Greenland...
Citation