Articles | Volume 22, issue 10
https://doi.org/10.5194/cp-22-1863-2026
© Author(s) 2026. This work is distributed under the Creative Commons Attribution 4.0 License.
Historical climate extremes in Europe and the connection between spring precipitation and summer heat
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- Final revised paper (published on 07 Oct 2026)
- Supplement to the final revised paper
- Preprint (discussion started on 11 Jun 2026)
- Supplement to the preprint
Interactive discussion
Status: closed
Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor
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RC1: 'Comment on egusphere-2026-2852', Olivier Planchon, 21 Jun 2026
- AC1: 'Reply on RC1', Stefan Bronnimann, 16 Aug 2026
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RC2: 'Comment on egusphere-2026-2852', Carla Mateus, 13 Jul 2026
- AC2: 'Reply on RC2', Stefan Bronnimann, 16 Aug 2026
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
ED: Submit a revised manuscript (24 Aug 2026) by Shiling Yang
AR by Stefan Bronnimann on behalf of the Authors (31 Aug 2026)
Author's response
Author's tracked changes
Manuscript
ED: Publish as is (08 Sep 2026) by Shiling Yang
AR by Stefan Bronnimann on behalf of the Authors (21 Sep 2026)
This particularly fascinating article proposes to go back 600 years in the past of Europe in order to identify, using proxy and instrumental data, reanalyses, and numerical simulations, whether the combination of certain spring weather / climate conditions is, significantly, heralding hot summers (a terribly topical subject!).
Given the quality of this work, I have no negative criticism to make. I would just like to ask a few questions and propose some suggestions to the authors, which may possibly improve the understanding of certain points and results that seem particularly interesting to me.
1) Would it be possible to specify what is the influence of the climatic context of the Little Ice Age (and its more or less severe / attenuated internal oscillations) on the frequency of atmospheric circulation types and their manifestations in terms of weather conditions highlighted in this study?
- NAO+ and NAO- phases;
- blocking patterns;
- occurrence of megadrought events.
2) Climatic conditions (interannual variability and multi-year alternately warm / cool oscillations) and atmospheric circulation that occurred during the transition between the end of the Little Ice Age and the period of contemporary global warming, did they influence certain results?
3) Possibility of an influence of the type of data used and analyzed on the results?
Compared to proxy data, what impacts and what importance could have precisely the measurements carried out from the seventeenth century onwards and their development (increasingly numerous across Europe) over the following centuries, in the analyses and on the results obtained in this work?
4) Among the questions asked by the authors themselves about highlighting characteristics specific to South-Eastern Europe climatology in the interpretation and understanding of the results, maybe the classification of atmospheric circulation patterns used in this work is not precise enough? If the classification used is relevant at the scale of the European continent, it is probably less so at smaller scales. Would the use of a more detailed classification such as that of Hess-Brezowsky circulation types (Großwetterlagen), if possible in the context of this work, be better suited to this regional scale?