Articles | Volume 13, issue 5
https://doi.org/10.5194/cp-13-437-2017
https://doi.org/10.5194/cp-13-437-2017
Research article
 | 
09 May 2017
Research article |  | 09 May 2017

A glaciochemical study of the 120 m ice core from Mill Island, East Antarctica

Mana Inoue, Mark A. J. Curran, Andrew D. Moy, Tas D. van Ommen, Alexander D. Fraser, Helen E. Phillips, and Ian D. Goodwin

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Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (07 Dec 2016) by Kumiko Goto-Azuma
AR by Mana Inoue on behalf of the Authors (08 Dec 2016)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (12 Dec 2016) by Kumiko Goto-Azuma
RR by Elisabeth Isaksson (06 Jan 2017)
RR by Anonymous Referee #1 (06 Feb 2017)
ED: Publish subject to technical corrections (19 Feb 2017) by Kumiko Goto-Azuma
AR by Mana Inoue on behalf of the Authors (27 Feb 2017)  Author's response   Manuscript 
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Short summary
A 120 m ice core from Mill Island, East Antarctica, was studied its chemical components. The Mill Island ice core contains 97 years of climate record (1913–2009) and has a mean snow accumulation of 1.35 m yr−1 (ice equivalent). Trace ion concentrations were generally higher than other Antarctic ice core sites. Nearby sea ice concentration was found to influence the annual mean sea salt record. The Mill Island ice core records are unexpectedly complex, with strong modulation of the trace chemistry.