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 2
The Cryosphere, 9, 663–673, 2015
https://doi.org/10.5194/tc-9-663-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
The Cryosphere, 9, 663–673, 2015
https://doi.org/10.5194/tc-9-663-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 09 Apr 2015

Research article | 09 Apr 2015

On producing sea ice deformation data sets from SAR-derived sea ice motion

S. Bouillon and P. Rampal
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 Sylvain Bouillon on behalf of the Authors (02 Feb 2015)  Author's response
ED: Referee Nomination & Report Request started (18 Feb 2015) by Daniel Feltham
RR by Anonymous Referee #2 (23 Feb 2015)
RR by Anonymous Referee #1 (01 Mar 2015)
ED: Publish subject to minor revisions (Editor review) (03 Mar 2015) by Daniel Feltham
AR by Sylvain Bouillon on behalf of the Authors (11 Mar 2015)  Author's response    Manuscript
ED: Publish as is (12 Mar 2015) by Daniel Feltham
Publications Copernicus
Download
Short summary
We present a new method to compute sea ice deformation fields from satellite-derived motion. The method particularly reduces the artificial noise that arises along discontinuities in the sea ice motion field. We estimate that this artificial noise may cause an overestimation of about 60% of sea ice opening and closing. The constant overestimation of the opening and closing could have led in previous studies to a large overestimation of freezing in leads, salt rejection and sea ice ridging.
We present a new method to compute sea ice deformation fields from satellite-derived motion. The...
Citation