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

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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Carmen Vega on behalf of the Authors (01 Mar 2016)
ED: Referee Nomination & Report Request started (09 Mar 2016) by Martin Schneebeli
ED: Publish subject to minor revisions (Editor review) (31 Mar 2016) by Martin Schneebeli
AR by Carmen Vega on behalf of the Authors (09 Apr 2016)  Manuscript 
ED: Publish as is (25 Apr 2016) by Martin Schneebeli
AR by Carmen Vega on behalf of the Authors (26 Apr 2016)
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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.