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degois.publication.firstPage17-
degois.publication.issue1-2pt_PT
degois.publication.titleClimatic Changept_PT
dc.relation.publisherversionhttps://link.springer.com/article/10.1007%2Fs10584-021-03039-7pt_PT
dc.contributor.authorAlcoforado, Maria Joao-
dc.contributor.authorSilva, Luís Pedro-
dc.contributor.authorAmorim, Inês-
dc.contributor.authorFragoso, Marcelo-
dc.contributor.authorGarcia, João Carlos-
dc.date.accessioned2021-06-25T14:33:29Z-
dc.date.available2021-06-25T14:33:29Z-
dc.date.issued2021-
dc.identifier.citationAlcoforado, M.J., Silva, L.P., Amorim, I., Fragoso, M. & Garcia, J. C. (2021). Historical floods of the Douro River in Porto, Portugal (1727–1799). Climatic Change 165, 17. https://doi.org/10.1007/s10584-021-03039-7pt_PT
dc.identifier.issn0165-0009-
dc.identifier.urihttp://hdl.handle.net/10451/48752-
dc.description.abstractExtreme meteorological events have had devastating consequences all over the world throughout the ages. In this study, we look into the floods at the mouth of the Douro River (Porto, Portugal) in the eighteenth century to expand the data series of floods in Northern Portugal. Information was gathered mostly from documentary narrative sources, either individual or institutional (administrative and ecclesiastic), some of which include reports of Pro Serenitate ceremonies. A study by the priest Rebelo Costa (1789) and the memories of the merchant Ignacio Henckell from 1717 to 1800 stand out among the individual sources. We concluded that there was great interannual variability in the occurrence of the 54 recorded floods, the highest number of which occurred in the 1780s. The “catastrophic” floods were recorded in 1727, 1739, 1769, 1774, 1777, 1788 and 1798, four of which are studied in detail in this paper. The greatest number of flood events took place in winter and autumn, and most of them lasted between 1 and 3 days. An analysis of the description of the floods, their impacts and the associated meteorological causes was carried out. In most cases, the frontal activity associated with Atlantic cyclonic systems was the cause of positive precipitation anomalies in NW Iberia. The great variability in heavy precipitation was confirmed by the new data. However, hardly any temporal simultaneity was found with other case studies in Southern Europe, except for Spain, especially several localities of Galicia and the mid Douro Valley (Zamora).pt_PT
dc.language.isoengpt_PT
dc.publisherSpringerpt_PT
dc.relationPTDC/AAC–CLI/119078/2010pt_PT
dc.relationinfo:eu-repo/grantAgreement/FCT/6817 - DCRRNI ID/UID%2FGEO%2F00295%2F2013/PTpt_PT
dc.relationUIDB/00295/2020 and UIDP/00295/2020pt_PT
dc.rightsopenAccesspt_PT
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/pt_PT
dc.subjectFloodspt_PT
dc.subjectMeteorological extremespt_PT
dc.subjectEighteenth centurypt_PT
dc.subjectDouro Riverpt_PT
dc.subjectPortopt_PT
dc.subjectPortugalpt_PT
dc.titleHistorical floods of the Douro River in Porto, Portugal (1727–1799)pt_PT
dc.typearticlept_PT
dc.description.versioninfo:eu-repo/semantics/publishedVersionpt_PT
dc.peerreviewedyespt_PT
degois.publication.volume165pt_PT
dc.identifier.doi10.1007/s10584-021-03039-7pt_PT
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