Articles | Volume 17, issue 5
https://doi.org/10.5194/cp-17-1841-2021
https://doi.org/10.5194/cp-17-1841-2021
Research article
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17 Sep 2021
Research article | Highlight paper |  | 17 Sep 2021

Enhanced moisture delivery into Victoria Land, East Antarctica, during the early Last Interglacial: implications for West Antarctic Ice Sheet stability

Yuzhen Yan, Nicole E. Spaulding, Michael L. Bender, Edward J. Brook, John A. Higgins, Andrei V. Kurbatov, and Paul A. Mayewski

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Review of Yan et al.', Frédéric Parrenin, 02 Mar 2021
    • RC3: 'Reply on RC1', Frédéric Parrenin, 03 Mar 2021
      • AC1: 'Reply to Dr. Parrenin', Yuzhen Yan, 05 May 2021
  • RC2: 'Comment on cp-2021-7', Anonymous Referee #2, 03 Mar 2021
    • AC2: 'Reply to two anonymous Referees', Yuzhen Yan, 05 May 2021
  • RC4: 'Review of Yan et al.', Anonymous Referee #3, 04 Mar 2021
    • AC2: 'Reply to two anonymous Referees', Yuzhen Yan, 05 May 2021
      • AC4: 'Reply on AC2', Yuzhen Yan, 05 May 2021
  • EC1: 'Editor comment on cp-2021-7', Eric Wolff, 08 Apr 2021
    • AC3: 'Reply on Editor', Yuzhen Yan, 05 May 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (06 May 2021) by Eric Wolff
AR by Yuzhen Yan on behalf of the Authors (22 Jun 2021)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (23 Jun 2021) by Eric Wolff
RR by Anonymous Referee #2 (31 Jul 2021)
ED: Publish subject to minor revisions (review by editor) (02 Aug 2021) by Eric Wolff
AR by Yuzhen Yan on behalf of the Authors (12 Aug 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (17 Aug 2021) by Eric Wolff
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Short summary
Here we reconstruct the rate of snow accumulation during the Last Interglacial period in an East Antarctic ice core located near the present-day northern edge of the Ross Ice Shelf. We find an order-of-magnitude increase in the accumulation rate during the peak warming in the Last Interglacial. This large increase in mass accumulation is compatible with less ice cover in the Ross Sea, perhaps created by a partly collapsed West Antarctic Ice Sheet, whose stability in a warming world is uncertain.