Articles | Volume 16, issue 5
https://doi.org/10.5194/esd-16-1539-2025
https://doi.org/10.5194/esd-16-1539-2025
Research article
 | 
24 Sep 2025
Research article |  | 24 Sep 2025

Bayesian analysis of early warning signals using a time-dependent model

Eirik Myrvoll-Nilsen, Luc Hallali, and Martin Rypdal

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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 egusphere-2024-436', Anonymous Referee #1, 14 Apr 2024
  • RC2: 'Comment on egusphere-2024-436', Anonymous Referee #2, 15 Apr 2024

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Reconsider after major revisions (12 Jul 2024) by Jonathan Donges
AR by Eirik Myrvoll-Nilsen on behalf of the Authors (23 Aug 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (11 Sep 2024) by Jonathan Donges
RR by Anonymous Referee #1 (26 Sep 2024)
RR by Chris Boulton (28 Mar 2025)
ED: Publish subject to minor revisions (review by editor) (01 Apr 2025) by Jonathan Donges
AR by Eirik Myrvoll-Nilsen on behalf of the Authors (11 Apr 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (12 Apr 2025) by Jonathan Donges
AR by Eirik Myrvoll-Nilsen on behalf of the Authors (19 Apr 2025)

Post-review adjustments

AA: Author's adjustment | EA: Editor approval
AA by Eirik Myrvoll-Nilsen on behalf of the Authors (08 Sep 2025)   Author's adjustment   Manuscript
EA: Adjustments approved (22 Sep 2025) by Jonathan Donges
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Short summary
Before a climate component reaches a tipping point, there may be observable changes in its statistical properties. These are known as early warning signals and include increased fluctuation and correlation times. We present a Bayesian approach to detect these signals, using a model where the correlation parameter depends linearly on time for which the slope can be estimated directly from the data. The model is then applied to Dansgaard–Oeschger events using Greenland ice core data.
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