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 10, issue 5
The Cryosphere, 10, 2173–2189, 2016
https://doi.org/10.5194/tc-10-2173-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
The Cryosphere, 10, 2173–2189, 2016
https://doi.org/10.5194/tc-10-2173-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 21 Sep 2016

Research article | 21 Sep 2016

Estimates of ikaite export from sea ice to the underlying seawater in a sea ice–seawater mesocosm

Nicolas-Xavier Geilfus et al.

Viewed

Total article views: 1,683 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
802 836 45 1,683 62 62
  • HTML: 802
  • PDF: 836
  • XML: 45
  • Total: 1,683
  • BibTeX: 62
  • EndNote: 62
Views and downloads (calculated since 11 Feb 2016)
Cumulative views and downloads (calculated since 11 Feb 2016)

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: 27 Feb 2020
Publications Copernicus
Download
Short summary
The fate of ikaite precipitation within sea ice is poorly understood. In this study, we estimated ikaite precipitation of up to 167 µmol kg-1 within sea ice, while its export and dissolution into the underlying seawater was responsible for a TA increase of 64–66 μmol kg-1. We estimated that more than half of the total ikaite precipitated was still contained in the ice when sea ice began to melt. The dissolution of the ikaite crystals in the water column kept the seawater pCO2 undersaturated.
The fate of ikaite precipitation within sea ice is poorly understood. In this study, we...
Citation