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 7
The Cryosphere, 12, 2383–2399, 2018
https://doi.org/10.5194/tc-12-2383-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
The Cryosphere, 12, 2383–2399, 2018
https://doi.org/10.5194/tc-12-2383-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 20 Jul 2018

Research article | 20 Jul 2018

Deglaciation and future stability of the Coats Land ice margin, Antarctica

Dominic A. Hodgson et al.
Viewed  
Total article views: 1,390 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
898 469 23 1,390 17 24
  • HTML: 898
  • PDF: 469
  • XML: 23
  • Total: 1,390
  • BibTeX: 17
  • EndNote: 24
Views and downloads (calculated since 06 Mar 2018)
Cumulative views and downloads (calculated since 06 Mar 2018)
Viewed (geographical distribution)  
Total article views: 1,241 (including HTML, PDF, and XML) Thereof 1,233 with geography defined and 8 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Cited  
Saved (final revised paper)  
No saved metrics found.
Saved (discussion paper)  
No saved metrics found.
Discussed (final revised paper)  
No discussed metrics found.
Discussed (discussion paper)  
No discussed metrics found.
Latest update: 14 Nov 2019
Publications Copernicus
Download
Short summary
We studied the Coats Land ice margin, Antarctica, providing a multi-disciplinary geophysical assessment of the ice sheet configuration through its last advance and retreat; a description of the physical constraints on the stability of the past and present ice and future margin based on its submarine geomorphology and ice-sheet geometry; and evidence that once detached from the bed, the ice shelves in this region were predisposed to rapid retreat back to coastal grounding lines.
We studied the Coats Land ice margin, Antarctica, providing a multi-disciplinary geophysical...
Citation