Articles | Volume 15, issue 7
The Cryosphere, 15, 3495–3505, 2021
https://doi.org/10.5194/tc-15-3495-2021
The Cryosphere, 15, 3495–3505, 2021
https://doi.org/10.5194/tc-15-3495-2021

Research article 27 Jul 2021

Research article | 27 Jul 2021

Reconstruction of annual accumulation rate on firn, synchronising H2O2 concentration data with an estimated temperature record

Jandyr M. Travassos et al.

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on tc-2020-342', Anonymous Referee #1, 11 Mar 2021
    • AC1: 'Reply on RC1', Saulo Martins, 10 Apr 2021
  • RC2: 'Comment on tc-2020-342', Anonymous Referee #2, 15 Mar 2021
    • AC2: 'Reply on RC2', Saulo Martins, 16 Apr 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (review by editor) (27 Apr 2021) by Michiel van den Broeke
AR by Saulo Martins on behalf of the Authors (02 May 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish subject to minor revisions (review by editor) (11 May 2021) by Michiel van den Broeke
AR by Saulo Martins on behalf of the Authors (20 May 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (21 May 2021) by Michiel van den Broeke

Post-review adjustments

AA: Author's adjustment | EA: Editor approval
AA by Saulo Martins on behalf of the Authors (13 Jul 2021)   Author's adjustment   Manuscript
EA: Adjustments approved (13 Jul 2021) by Michiel van den Broeke
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Short summary
This paper gives a timescale estimation and the yearly accumulation rate from ice cores encompassing the entire firn layer at the Detroit Plateau, the Antarctic Peninsula, through a non-linear pairing transformation of high-resolution H2O2 concentration data to a local temperature time series. An 11-year moving average of the yearly ice accumulation rate may suggest an increase in the span of 30 years, with an average of 2.5–2.8 m w.e./year.