Articles | Volume 11, issue 2
The Cryosphere, 11, 693–705, 2017
https://doi.org/10.5194/tc-11-693-2017
The Cryosphere, 11, 693–705, 2017
https://doi.org/10.5194/tc-11-693-2017

Research article 17 Mar 2017

Research article | 17 Mar 2017

Bromine, iodine and sodium in surface snow along the 2013 Talos Dome–GV7 traverse (northern Victoria Land, East Antarctica)

Niccolò Maffezzoli et al.

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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
AR by Niccolò Maffezzoli on behalf of the Authors (17 Jan 2017)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (22 Jan 2017) by Joel Savarino
RR by Legrand Michel (04 Feb 2017)
RR by Anonymous Referee #2 (07 Feb 2017)
ED: Publish subject to minor revisions (Editor review) (07 Feb 2017) by Joel Savarino
AR by Niccolò Maffezzoli on behalf of the Authors (08 Feb 2017)  Author's response    Manuscript
ED: Publish as is (09 Feb 2017) by Joel Savarino
AR by Niccolò Maffezzoli on behalf of the Authors (11 Feb 2017)  Author's response    Manuscript
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Short summary
Sea ice is a crucial parameter within Earth's climate system. Understanding its dynamics and its response to other climatic variables is therefore of primary importance in view of a warming climate and sea ice decline. In this work we investigate some features of a chemical parameter in ice cores, bromine enrichment, which is linked to sea ice and can therefore be used to reconstruct sea ice in the past.