Preprints
https://doi.org/10.5194/egusphere-2025-1042
https://doi.org/10.5194/egusphere-2025-1042
02 Apr 2025
 | 02 Apr 2025

Strong wind occurrence in Poland from the 13th to 16th centuries based on documentary evidence

Rajmund Przybylak, Andrzej Araźny, Janusz Filipiak, Piotr Oliński, Przemysław Wyszyński, and Artur Szwaba

Abstract. A comprehensive database of strong winds based on documentary evidence was created for Poland until AD 1600. Three types of documentary sources were used: handwritten and unpublished, published, and “secondary” literature. The database contains detailed information about the occurrence of strong winds (the location/region, time, duration and indexation for intensity, extent and character of damage), as well as the exact textual content of the original weather note, the name of the source, and an evaluation of the source’s quality. Five categories of strong winds were delimited: 1 − fresh and strong breeze (Beaufort scale 5–7), 2 − gale (8–9), 3 − storm (10–12), 4 − squall (i.e., gusty wind during a thunderstorm), and 5 – tornadoes. The intensity, extent, and character of damage were estimated based on the proposition given by Brázdil et al. (2004), which we slightly modified to include the Baltic Sea and its influence on coastal parts. In the database, 137 thus-defined strong winds were identified. A reliable estimate of some characteristics of the occurrence of strong winds in Poland seems possible from the mid-15th century onwards. The highest number of strong winds occurred in the second half of the 16th century, with a maximum in the 1570s. For each season, the greatest number of strong winds was found for the Baltic Coast and Pomerania region, and then for Silesia and Lesser Poland. Storms and gales were most common during the cold half-year (mainly in March, November, and December).

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Journal article(s) based on this preprint

04 Sep 2025
Strong wind occurrence in Poland from the 13th to 16th centuries based on documentary evidence
Rajmund Przybylak, Andrzej Araźny, Janusz Filipiak, Piotr Oliński, Przemysław Wyszyński, and Artur Szwaba
Clim. Past, 21, 1501–1519, https://doi.org/10.5194/cp-21-1501-2025,https://doi.org/10.5194/cp-21-1501-2025, 2025
Short summary
Rajmund Przybylak, Andrzej Araźny, Janusz Filipiak, Piotr Oliński, Przemysław Wyszyński, and Artur Szwaba

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2025-1042', Anonymous Referee #1, 30 Apr 2025
  • RC2: 'Comment on egusphere-2025-1042', Anonymous Referee #2, 26 May 2025

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2025-1042', Anonymous Referee #1, 30 Apr 2025
  • RC2: 'Comment on egusphere-2025-1042', Anonymous Referee #2, 26 May 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) (09 Jun 2025) by Francesco Muschitiello
AR by Przemyslaw Wyszynski on behalf of the Authors (13 Jun 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (18 Jun 2025) by Francesco Muschitiello
AR by Przemyslaw Wyszynski on behalf of the Authors (20 Jun 2025)  Manuscript 

Journal article(s) based on this preprint

04 Sep 2025
Strong wind occurrence in Poland from the 13th to 16th centuries based on documentary evidence
Rajmund Przybylak, Andrzej Araźny, Janusz Filipiak, Piotr Oliński, Przemysław Wyszyński, and Artur Szwaba
Clim. Past, 21, 1501–1519, https://doi.org/10.5194/cp-21-1501-2025,https://doi.org/10.5194/cp-21-1501-2025, 2025
Short summary
Rajmund Przybylak, Andrzej Araźny, Janusz Filipiak, Piotr Oliński, Przemysław Wyszyński, and Artur Szwaba
Rajmund Przybylak, Andrzej Araźny, Janusz Filipiak, Piotr Oliński, Przemysław Wyszyński, and Artur Szwaba

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Short summary
A comprehensive database of strong winds based on documentary evidence was created for Poland until AD 1600. Three types of documentary sources were used: handwritten and unpublished, published, and “secondary” literature. The database contains detailed information about the occurrence of strong winds (the location/region, time, duration and indexation for intensity, extent and character of damage), as well as the exact textual content of the original weather note.
Share