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 12, issue 4
The Cryosphere, 12, 1157–1176, 2018
https://doi.org/10.5194/tc-12-1157-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
The Cryosphere, 12, 1157–1176, 2018
https://doi.org/10.5194/tc-12-1157-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 04 Apr 2018

Research article | 04 Apr 2018

Canadian snow and sea ice: historical trends and projections

Lawrence R. Mudryk et al.

Viewed

Total article views: 2,724 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,602 1,068 54 2,724 43 61
  • HTML: 1,602
  • PDF: 1,068
  • XML: 54
  • Total: 2,724
  • BibTeX: 43
  • EndNote: 61
Views and downloads (calculated since 09 Oct 2017)
Cumulative views and downloads (calculated since 09 Oct 2017)

Viewed (geographical distribution)

Total article views: 2,403 (including HTML, PDF, and XML) Thereof 2,398 with geography defined and 5 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Saved (final revised paper)

No saved metrics found.

Saved (preprint)

No saved metrics found.

Discussed (final revised paper)

Discussed (preprint)

No discussed metrics found.
Latest update: 01 Jun 2020
Publications Copernicus
Short summary
This paper presents changes in both snow and sea ice that have occurred over Canada during the recent past and shows climate model estimates for future changes expected to occur by the year 2050. The historical changes of snow and sea ice are generally coherent and consistent with the regional history of temperature and precipitation changes. It is expected that snow and sea ice will continue to decrease in the future, declining by an additional 15–30 % from present day values by the year 2050.
This paper presents changes in both snow and sea ice that have occurred over Canada during the...
Citation