Articles | Volume 20, issue 5
https://doi.org/10.5194/cp-20-1213-2024
https://doi.org/10.5194/cp-20-1213-2024
Research article
 | 
28 May 2024
Research article |  | 28 May 2024

Drivers of late Holocene ice core chemistry in Dronning Maud Land: the context for the ISOL-ICE project

V. Holly L. Winton, Robert Mulvaney, Joel Savarino, Kyle R. Clem, and Markus M. Frey

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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 cp-2023-96', Anonymous Referee #1, 16 Jan 2024
  • RC2: 'Comment on cp-2023-96', Tessa Vance, 09 Feb 2024

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) (05 Apr 2024) by Hubertus Fischer
AR by Holly Winton on behalf of the Authors (08 Apr 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to technical corrections (09 Apr 2024) by Hubertus Fischer
AR by Holly Winton on behalf of the Authors (10 Apr 2024)  Manuscript 
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Short summary
In 2018, a new 120 m ice core was drilled in a region located under the Antarctic ozone hole. We present the first results including a 1300-year record of snow accumulation and aerosol chemistry. We investigate the aerosol and moisture source regions and atmospheric processes related to the ice core record and discuss what this means for developing a record of past ultraviolet radiation and ozone depletion using the stable isotopic composition of nitrate measured in the same ice core.