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

Journal metrics

Journal metrics

  • IF value: 4.713 IF 4.713
  • IF 5-year value: 4.927 IF 5-year
    4.927
  • CiteScore value: 8.0 CiteScore
    8.0
  • SNIP value: 1.425 SNIP 1.425
  • IPP value: 4.65 IPP 4.65
  • SJR value: 2.353 SJR 2.353
  • Scimago H <br class='hide-on-tablet hide-on-mobile'>index value: 71 Scimago H
    index 71
  • h5-index value: 53 h5-index 53
TC | Articles | Volume 14, issue 5
The Cryosphere, 14, 1703–1712, 2020
https://doi.org/10.5194/tc-14-1703-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
The Cryosphere, 14, 1703–1712, 2020
https://doi.org/10.5194/tc-14-1703-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 29 May 2020

Research article | 29 May 2020

Horizontal ice flow impacts the firn structure of Greenland's percolation zone

Rosemary Leone et al.

Viewed

Total article views: 1,161 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
938 208 15 1,161 50 20 14
  • HTML: 938
  • PDF: 208
  • XML: 15
  • Total: 1,161
  • Supplement: 50
  • BibTeX: 20
  • EndNote: 14
Views and downloads (calculated since 24 Oct 2019)
Cumulative views and downloads (calculated since 24 Oct 2019)

Viewed (geographical distribution)

Total article views: 761 (including HTML, PDF, and XML) Thereof 760 with geography defined and 1 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)

No discussed metrics found.

Discussed (preprint)

No discussed metrics found.
Latest update: 05 Aug 2020
Publications Copernicus
Download
Short summary
Horizontal ice flow transports the firn layer of Greenland’s Percolation Zone as it undergoes burial by accumulation. Here we show that the firn density and temperature fields can reflect horizontal advection of the firn column across climate gradients, the magnitude of which varies around the ice sheet. Further, time series of melt features in ice cores from the percolation zone can contain a signature from ice motion that should not be conflated with that from climate change.
Horizontal ice flow transports the firn layer of Greenland’s Percolation Zone as it undergoes...
Citation