Articles | Volume 18, issue 5
https://doi.org/10.5194/cp-18-989-2022
https://doi.org/10.5194/cp-18-989-2022
Research article
 | 
06 May 2022
Research article |  | 06 May 2022

Reorganization of Atlantic Waters at sub-polar latitudes linked to deep-water overflow in both glacial and interglacial climate states

Dakota E. Holmes, Tali L. Babila, Ulysses Ninnemann, Gordon Bromley, Shane Tyrrell, Greig A. Paterson, Michelle J. Curran, and Audrey Morley

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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 cp-2021-97', Christoph Nehrbass-Ahles, 24 Aug 2021
    • AC1: 'Reply on CC1', Audrey Morley, 31 Aug 2021
  • RC1: 'Comment on cp-2021-97', Ian Candy, 29 Aug 2021
  • RC2: 'Comment on cp-2021-97', Anonymous Referee #2, 30 Aug 2021
  • RC3: 'Comment on cp-2021-97', Anonymous Referee #3, 06 Sep 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (11 Nov 2021) by David Thornalley
AR by Audrey Morley on behalf of the Authors (24 Dec 2021)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (17 Jan 2022) by David Thornalley
RR by Anonymous Referee #3 (08 Feb 2022)
RR by Daniel Parkes (02 Mar 2022)
ED: Publish subject to minor revisions (review by editor) (05 Mar 2022) by David Thornalley
AR by Audrey Morley on behalf of the Authors (15 Mar 2022)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (21 Mar 2022) by David Thornalley
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Short summary
Our proxy-based observations of the glacial inception following MIS 11 advance our mechanistic understanding of (and elucidates antecedent conditions that can lead to) high-magnitude climate instability during low- and intermediate-ice boundary conditions. We find that irrespective of the magnitude of climate variability or boundary conditions, the reorganization between Polar Water and Atlantic Water at subpolar latitudes appears to influence deep-water flow in the Nordic Seas.