Articles | Volume 26, issue 5
https://doi.org/10.5194/nhess-26-2051-2026
© Author(s) 2026. This work is distributed under the Creative Commons Attribution 4.0 License.
The relationships between extreme winter North Atlantic extratropical cyclone hazards and modes of seasonal climate variability
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- Final revised paper (published on 08 May 2026)
- Supplement to the final revised paper
- Preprint (discussion started on 24 Mar 2025)
- Supplement to the preprint
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 egusphere-2025-1131', Mika Rantanen, 16 Apr 2025
- AC1: 'Reply on RC1', Amanda Maycock, 11 Aug 2025
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RC2: 'Comment on egusphere-2025-1131', Anonymous Referee #2, 28 Apr 2025
- AC3: 'Reply on RC2', Amanda Maycock, 11 Aug 2025
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RC3: 'Comment on egusphere-2025-1131', Lisa Degenhardt, 29 Apr 2025
- AC2: 'Reply on RC3', Amanda Maycock, 11 Aug 2025
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
ED: Reconsider after major revisions (further review by editor and referees) (16 Sep 2025) by Joaquim G. Pinto
AR by Amanda Maycock on behalf of the Authors (08 Jan 2026)
Author's response
Author's tracked changes
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ED: Referee Nomination & Report Request started (11 Jan 2026) by Joaquim G. Pinto
RR by Mika Rantanen (21 Jan 2026)
RR by Anonymous Referee #2 (02 Feb 2026)
ED: Publish subject to minor revisions (review by editor) (06 Feb 2026) by Joaquim G. Pinto
AR by Amanda Maycock on behalf of the Authors (23 Feb 2026)
Author's response
Author's tracked changes
Manuscript
ED: Publish subject to technical corrections (25 Feb 2026) by Joaquim G. Pinto
AR by Amanda Maycock on behalf of the Authors (14 Mar 2026)
Manuscript
Review of NHESSD manuscript egusphere-2025-1131 “North Atlantic seasonal climate variability significantly modulates extreme winter Euro-Atlantic extratropical cyclone hazards” by Maycock et al.
This paper investigates the relationship between large-scale climate modes and ETC-related hazards in Europe. The authors track cyclones, calculate their hazard footprints and then use linear regression to find how much the ETC-related extremes change with respect to PC1 (North Atlantic Oscillation) and PC2 (East Atlantic pattern). The key result is that PC1 or PC2 alone exhibit increases in hazards in relatively different geographical areas (i.e. PC1 in the east and north of the UK, but PC2 mainly in the west and south). In addition, there are areas which exhibit signals for several hazards at the same time, and areas where both PC1 and PC2 affect simultaneously.
I like the research idea and I think this is definitely something which is worth publishing in NHESS. The used datasets are appropriate for conducting this kind of study. I also liked that negative results (SDI) were mentioned.
However, I had some concerns related to how the key results are presented. I think this could have been done in a more explicit/quantitative way (see comment 1). In addition, I’m afraid that the daily precipitation associated with the ETCs might be overestimated (see comment 2). I hope that the authors could address these concerns before the publication of this study.
Major comments:
Other comments:
Section 2. It seems that the whole analysis is restricted to the NH winter but it would be good to mention the months (Dec-Feb) explicitly in the Methods section. Currently, this is mentioned only in Section 2.3 but I guess it applies to the whole analysis. Which leads me to the 2nd question. Why only DJF? At least in Fennoscandia, November is often a very active month in terms of windstorm hazards.
Section 2.3. North Atlantic modes of variability. I think section 2.3 is a bit incomplete. It lacks justification why you chose the domain which you chose (90W-40E, 20-80N). Furthermore, I think this area is often called the Euro-Atlantic sector as it extends up to 40E, but you talk about the North Atlantic sector which is slightly misleading, given the area. Also, some studies (e.g. https://rmets.onlinelibrary.wiley.com/doi/10.1002/qj.3341) call the 2nd EOF as Scandinavian or European blocking. Is the East Atlantic pattern the same as Scandinavian blocking? If not, it might be reasonable to mention this in the text. It might help if the regression/correlation patterns against MSLP are shown, for example in supplementary material.
Section 4. Please consider writing something about the limitations of your analysis. For example, the linear model does not naturally explain all the variability in ETC-related hazards. What other factors are there which add the variability? How could you improve your work in the future?
L46 and thereafter. You often cite Degenhardt et al. 2022 but there is only Degenhardt et al. 2023 and 2024 in the reference list.
L136. This should be Section 2.4
L155: these metrics? which metrics?
L157: Here you mention that linear regression performs poorly if the data is non-linear and contains lots of zeros. But isn’t that the case for ETC-hazards too, for those regions which infrequently see ETCs during DJF months? So how do you deal with those regions that are far from storm tracks, and might not see ETCs every winter? Are there those regions at all?
L182: are shown
L200: show a reduction? How can you see this as the colour bars in Fig. 3 only show positive values? I see that the absolute anomalies in Fig. S3 also have negative values, but I don't understand why the percentage anomalies in the ΔPC1 and ΔPC2 maps in Fig. 3 only show positive changes?
L287. Previous work. Here it would be good to cite the actual previous work.
Fig. 5 and 6: the titles show 1981-2010, should it be 2020? And why does Fig. 7 have 2021 in its title?