Articles | Volume 7-osr10
https://doi.org/10.5194/sp-7-osr10-16-2026
© Author(s) 2026. This work is distributed under the Creative Commons Attribution 4.0 License.
Record low sea levels in the Bothnian Bay in November 2024
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- Final revised paper (published on 30 Sep 2026)
- Preprint (discussion started on 19 Sep 2025)
Interactive discussion
Status: closed
Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor
| : Report abuse
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RC1: 'Comment on sp-2025-12', Anonymous Referee #1, 27 Oct 2025
- AC1: 'Reply on RC1', Laura Tuomi, 17 Dec 2025
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RC2: 'Comment on sp-2025-12', Anonymous Referee #2, 12 Nov 2025
- AC2: 'Reply on RC2', Laura Tuomi, 17 Dec 2025
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
ED: Publish subject to minor revisions (review by editor) (05 Jan 2026) by Johannes Karstensen
AR by Laura Tuomi on behalf of the Authors (26 Jan 2026)
Author's response
Author's tracked changes
Manuscript
ED: Publish subject to technical corrections (03 Feb 2026) by Johannes Karstensen
ED: Publish subject to technical corrections (10 Feb 2026) by Marilaure Grégoire (Chief editor)
AR by Laura Tuomi on behalf of the Authors (18 Feb 2026)
Manuscript
Summary: The manuscript presents a characterisation of an extreme low sea level in the Gulf of Bosnia in the Baltic Sea. The magnitude of this extreme was exceptional compared to the past historical record. This extreme event was linked to winds flowing from a specific direction. The study estimated the return period of this extreme and assessed the short-term forecast for it.
Recommendation: The manuscript is clearly written, and the analysis is, in my opinion, correctly conducted. I have, however, some concerns about the suitability of the topic for the journal, a decision that the editor or the editorial board should make. The manuscript presents an analysis of a very specific sea-level extreme. This assessment may certainly be relevant from the operational meteorological or oceanographic point of view, but I do not clearly see its impact as an assessment report for 'State of the Planet'
Leaving this question aside, I have a few suggestions that the authors may want to consider:
1) The abstract indicates some sea-level figures to characterise the magnitude of the extreme, but these are only meaningful to researchers working specifically in this geographical area. Also, it would be more useful to indicate the magnitude in terms of standard deviations derived from some climatological period (possibly detrended to subtract the impact of the GIA)
2) The Abstract should also mention the exact date of the extreme. This is first mentioned at the end of the introduction.
3) line 96 'We present winds measured at Kalajoki...' daily, hourly, 6-hourly..?
4) The resolution of Figure 1 should be improved.
5) line 170 'forecast lengths'
I think the authors mean forecast horizons. For instance, the length of a forecast be 10 days if it s continued beyond the forecast horizon of , say 1 24 hours.
6) The GEV analysis is correctly conducted using detrended data. It is interesting to know whether November 21th remains a record sea level even in the detrended series
7) A GEV analysis of the winds, for instance, daily means, would also be interesting. It would address the question of whether the sea-level record was due solely to the magnitude of the winds, or to some combination of strong winds, the prefilling state, or sea-ice cover.
8) What were the sea-ice cover conditions? Ice cover is known to modulate the amount of momentum transferred from the atmosphere to the ocean. Did a smaller-than-normal ice cover play a role? Somewhat surprisingly, ice cover is not mentioned at all in the manuscript (or I missed it). This would increase the 'climatological aspect' of the study and perhaps make it more suitable for publication in State of the Planet