Articles | Volume 17, issue 12
https://doi.org/10.5194/tc-17-5155-2023
https://doi.org/10.5194/tc-17-5155-2023
Research article
 | 
06 Dec 2023
Research article |  | 06 Dec 2023

Identifying atmospheric processes favouring the formation of bubble-free layers in the Law Dome ice core, East Antarctica

Lingwei Zhang, Tessa R. Vance, Alexander D. Fraser, Lenneke M. Jong, Sarah S. Thompson, Alison S. Criscitiello, and Nerilie J. Abram

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • CC1: 'Comment on egusphere-2023-611', D.A. Winski, 22 May 2023
  • RC1: 'Comment on egusphere-2023-611', Dominic Winski, 24 May 2023
  • RC2: 'Review of egusphere-2023-611', Anonymous Referee #2, 05 Jul 2023

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish subject to minor revisions (review by editor) (07 Aug 2023) by Alexis LAMOTHE
AR by Lingwei Zhang on behalf of the Authors (03 Oct 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (14 Oct 2023) by Alexis LAMOTHE
AR by Lingwei Zhang on behalf of the Authors (25 Oct 2023)  Manuscript 
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Short summary
Physical features in ice cores provide unique records of past variability. We identified 1–2 mm ice layers without bubbles in surface ice cores from Law Dome, East Antarctica, occurring on average five times per year. The origin of these bubble-free layers is unknown. In this study, we investigate whether they have the potential to record past atmospheric processes and circulation. We find that the bubble-free layers are linked to accumulation hiatus events and meridional moisture transport.