Articles | Volume 21, issue 2
https://doi.org/10.5194/cp-21-593-2025
https://doi.org/10.5194/cp-21-593-2025
Research article
 | 
28 Feb 2025
Research article |  | 28 Feb 2025

Assessing the most severe subsistence crisis of the 18th century in the northwest of the Iberian Peninsula: a climatological perspective

Maite deCastro, José González-Cao, Nicolás G. deCastro, Juan J. Taboada, José M. Vaquero, and Moncho Gómez-Gesteira

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • CC1: 'Comment on cp-2024-49- A short comment on the title and Figs 4,5, and 6', Zoltán Kern, 17 Oct 2024
    • CC2: 'Reply on CC1', Maite deCastro, 17 Oct 2024
    • AC1: 'Reply on CC1', Maite deCastro, 12 Dec 2024
  • RC1: 'Comment on cp-2024-49', Anonymous Referee #1, 09 Nov 2024
    • CC3: 'Reply on RC1', Maite deCastro, 11 Nov 2024
    • AC1: 'Reply on CC1', Maite deCastro, 12 Dec 2024
    • AC2: 'Reply on RC1', Maite deCastro, 12 Dec 2024
  • RC2: 'Comment on cp-2024-49', Anonymous Referee #2, 10 Nov 2024

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Reconsider after major revisions (13 Dec 2024) by Hugues Goosse
AR by Maite deCastro on behalf of the Authors (14 Dec 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (16 Dec 2024) by Hugues Goosse
RR by Anonymous Referee #1 (03 Jan 2025)
ED: Publish subject to technical corrections (06 Jan 2025) by Hugues Goosse
AR by Maite deCastro on behalf of the Authors (08 Jan 2025)  Author's response   Manuscript 
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Short summary
Persistent rains in the eastern Atlantic during 1768–1769 caused the worst agricultural crisis in Galicia and northern Portugal. Using the EKF400v2 paleo-reanalysis dataset, it was found that the rainfall anomaly was positive in 11 out of 12 months. June 1768 saw the highest positive rain anomaly of the century; September 1768 saw the second-highest. The atmospheric synoptic patterns show negative anomalies in sea level pressure and 500 hPa. These patterns induce surface low-pressure systems.

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