Articles | Volume 18, issue 8
Clim. Past, 18, 1831–1847, 2022
https://doi.org/10.5194/cp-18-1831-2022
Clim. Past, 18, 1831–1847, 2022
https://doi.org/10.5194/cp-18-1831-2022
Research article
10 Aug 2022
Research article | 10 Aug 2022

The ST22 chronology for the Skytrain Ice Rise ice core – Part 1: A stratigraphic chronology of the last 2000 years

Helene M. Hoffmann 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 cp-2022-28', Anonymous Referee #1, 13 Apr 2022
    • AC1: 'Reply on RC1', Helene Hoffmann, 23 Jun 2022
  • RC2: 'Comment on cp-2022-28', Anders Svensson, 12 May 2022
    • AC2: 'Reply on RC2', Helene Hoffmann, 23 Jun 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (05 Jul 2022) by Barbara Stenni
AR by Helene Hoffmann on behalf of the Authors (13 Jul 2022)  Author's response    Author's tracked changes    Manuscript
ED: Publish subject to technical corrections (17 Jul 2022) by Barbara Stenni
AR by Helene Hoffmann on behalf of the Authors (20 Jul 2022)  Author's response    Manuscript
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Short summary
The WACSWAIN project (WArm Climate Stability of the West Antarctic ice sheet in the last INterglacial) investigates the fate of the West Antarctic Ice Sheet during the last warm period on Earth (115 000–130 000 years before present). Within this framework an ice core was recently drilled at Skytrain Ice Rise. In this study we present a stratigraphic chronology of that ice core based on absolute age markers and annual layer counting for the last 2000 years.