Articles | Volume 22, issue 7
https://doi.org/10.5194/cp-22-1255-2026
© Author(s) 2026. This work is distributed under the Creative Commons Attribution 4.0 License.
Climate variability in Poland (Central Europe) in the 16th century based on multiproxy data
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- Final revised paper (published on 06 Jul 2026)
- Supplement to the final revised paper
- Preprint (discussion started on 06 Mar 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-2026-1172', Olivier Planchon, 19 Mar 2026
- AC1: 'Reply on RC1', Aleksandra Pospieszynska, 20 May 2026
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RC2: 'Comment on egusphere-2026-1172', Anonymous Referee #2, 06 Apr 2026
- AC2: 'Reply on RC2', Aleksandra Pospieszynska, 20 May 2026
- AC3: 'Reply on RC2', Aleksandra Pospieszynska, 20 May 2026
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AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
ED: Publish subject to minor revisions (review by editor) (20 May 2026) by Jürg Luterbacher
AR by Aleksandra Pospieszynska on behalf of the Authors (29 May 2026)
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ED: Publish as is (29 May 2026) by Jürg Luterbacher
AR by Aleksandra Pospieszynska on behalf of the Authors (03 Jun 2026)
This paper is placed in the context of numerous other publications dealing with the study of climatic conditions during the Little Ice Age in Western and Central Europe, by means of the combined analysis of dendrochronological data and documentary sources. The major interest of the results obtained is to confirm, on the territory of present-day Poland, the complexity of the climatic history at that time. The authors clearly show the existence of multi-year oscillations, both thermal and pluviometric, and sometimes contradict, in a very relevant way, the notion of the Little Ice Age as it is usually understood. Interannual climate variability is therefore highlighted, modulated according to the seasons. Seasonality seems to me, in this article, to be one of the most interesting points, because the authors highlight a continental character of the climate more accentuated than nowadays. Continentality is more rarely studied than the mere temporal evolution of temperature, which makes this point particularly interesting to study and develop, perhaps for a possible follow-up to this article? Many ''continentality indices'' have been developed for more than a century to quantify continentality using various parameters. Perhaps it would be relevant to use some of them for studies of palaeoclimatic reconstructions?
Two other questions for the authors:
- Among the documentary sources used, did the authors have in hand information concerning possible links between weather / climate conditions and agricultural activities, for example harvest dates and/or indications of yields and damage to certain crops?
- At that time, did the administration of the Hanseatic city of Danzig carry out systematic observations of the winter freeze-up of its port and gulf, like its ''colleagues'' in Riga?