Articles | Volume 10, issue 3
https://doi.org/10.5194/tc-10-961-2016
https://doi.org/10.5194/tc-10-961-2016
Research article
 | 
11 May 2016
Research article |  | 11 May 2016

A synthetic ice core approach to estimate ion relocation in an ice field site experiencing periodical melt: a case study on Lomonosovfonna, Svalbard

Carmen P. Vega, Veijo A. Pohjola, Emilie Beaudon, Björn Claremar, Ward J. J. van Pelt, Rickard Pettersson, Elisabeth Isaksson, Tõnu Martma, Margit Schwikowski, and Carl E. Bøggild

Viewed

Total article views: 2,984 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,502 1,306 176 2,984 154 148
  • HTML: 1,502
  • PDF: 1,306
  • XML: 176
  • Total: 2,984
  • BibTeX: 154
  • EndNote: 148
Views and downloads (calculated since 29 Sep 2015)
Cumulative views and downloads (calculated since 29 Sep 2015)

Cited

Discussed (final revised paper)

Latest update: 16 Jun 2024
Download
Short summary
To quantify post-depositional relocation of major ions by meltwater in snow and firn at Lomonosovfonna, Svalbard, consecutive ice cores drilled at this site were used to construct a synthetic core. The relocation length of most of the ions was on the order of 1 m between 2007 and 2010. Considering the ionic relocation lengths and annual melt percentages, we estimate that the atmospheric ionic signal remains preserved in recently drilled Lomonosovfonna ice cores at an annual or bi-annual resolution.