Articles | Volume 17, issue 6
Clim. Past, 17, 2653–2677, 2021
https://doi.org/10.5194/cp-17-2653-2021
Clim. Past, 17, 2653–2677, 2021
https://doi.org/10.5194/cp-17-2653-2021

Research article 22 Dec 2021

Research article | 22 Dec 2021

Hydroclimatic variability of opposing Late Pleistocene climates in the Levant revealed by deep Dead Sea sediments

Yoav Ben Dor 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-2020-161', Anonymous Referee #1, 09 Feb 2021
    • AC2: 'Reply on RC1', Yoav Ben Dor, 24 Jun 2021
  • RC2: 'Review of the Manuscript entitled “Hydroclimatic variability of opposing late Pleistocene climates in the Levant revealed by Dead Sea sediments” by Yoav Ben Dor and co-authors.', Anonymous Referee #2, 16 Feb 2021
    • AC3: 'Reply on RC2', Yoav Ben Dor, 24 Jun 2021
  • RC3: 'Review of Ben Dor et al. - Methodological aspects', Reik Donner, 13 Apr 2021
    • AC4: 'Reply on RC3', Yoav Ben Dor, 24 Jun 2021
  • EC1: 'Comment on cp-2020-161', Pierre Francus, 14 Apr 2021
    • AC1: 'Reply on EC1', Yoav Ben Dor, 24 Jun 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (25 Jun 2021) by Pierre Francus
AR by Yoav Ben Dor on behalf of the Authors (11 Aug 2021)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (17 Sep 2021) by Pierre Francus
RR by Reik Donner (31 Oct 2021)
ED: Publish subject to minor revisions (review by editor) (08 Nov 2021) by Pierre Francus
AR by Yoav Ben Dor on behalf of the Authors (26 Nov 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (29 Nov 2021) by Pierre Francus
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Short summary
Laminated sediments from the deepest part of the Dead Sea unravel the hydrological response of the eastern Mediterranean to past climate changes. This study demonstrates the importance of geological archives in complementing modern hydrological measurements that do not fully capture natural hydroclimatic variability, which is crucial to configure for understanding the impact of climate change on the hydrological cycle in subtropical regions.