Articles | Volume 12, issue 4
The Cryosphere, 12, 1177–1194, 2018
https://doi.org/10.5194/tc-12-1177-2018
The Cryosphere, 12, 1177–1194, 2018
https://doi.org/10.5194/tc-12-1177-2018

Research article 05 Apr 2018

Research article | 05 Apr 2018

Nitrate deposition and preservation in the snowpack along a traverse from coast to the ice sheet summit (Dome A) in East Antarctica

Guitao Shi 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 Guitao Shi on behalf of the Authors (13 Jan 2018)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (15 Jan 2018) by Joel Savarino
RR by Anonymous Referee #1 (16 Jan 2018)
ED: Publish subject to minor revisions (review by editor) (23 Jan 2018) by Joel Savarino
AR by Guitao Shi on behalf of the Authors (30 Jan 2018)  Author's response    Manuscript
ED: Publish subject to technical corrections (06 Feb 2018) by Joel Savarino
AR by Guitao Shi on behalf of the Authors (13 Feb 2018)  Author's response    Manuscript

Post-review adjustments

AA: Author's adjustment | EA: Editor approval
AA by Guitao Shi on behalf of the Authors (27 Mar 2018)   Author's adjustment   Manuscript
EA: Adjustments approved (02 Apr 2018) by Joel Savarino
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Short summary
The deposition and preservation of NO3 across East Antarctica was investigated. On the coast, dry deposition contributes 27–44 % of the NO3 fluxes, and the linear relationship between NO3 and snow accumulation rate suggests a homogeneity of atmospheric NO3 levels. In inland snow, a relatively weak correlation between NO3 and snow accumulation was found, indicating that NO3 is mainly dominated by post-depositional processes. The coexisting ions are generally less influential on snow NO3.