A 1400-years flood frequency reconstruction for the Basque country (N Spain): Integrating geological, historical and instrumental datasets

J. P. Corella, G. Benito, A. P. Monteoliva, J. Sigro, M. Calle, B. L. Valero-Garcés, V. Stefanova, E. Rico, A. C. Favre, B. Wilhelm

Research output: Contribution to journalArticlepeer-review

Abstract

We present the first reconstruction of past flood events variability in the Basque Country and Western Ebro Basin (Northern Spain) integrating instrumental hydrological datasets (last 20 years), documentary archives (last 700 years) and Lake Arreo (655 m a.s.l.) sedimentary paleoflood record (last 1400 years). In this lake, allochthonous coarse and fine detrital layers (CDL and FDL respectively) intercalated within endogenic laminites were identified and interpreted as high- and moderate-energy flood events. The interplay between human activities and hydroclimate variability has controlled the deposition of these flood layers. Gauged data for the last 20 years suggest that floods are typically generated by heavy rainfall events on saturated soils after several days of continuous rainfall. These events occur mostly during the cold season (Oct–May). The reconstructed frequency of high-magnitude flood events from the lake record is coherent with the historical cold-season floods from Basque rivers. The lowest flood frequency took place during the 6–7th and 10–15th centuries, while higher flood frequency occurred during the 8–9th centuries and the last 500 years. Fluvial and lacustrine paleoflood records and documentary evidence show abrupt and large increases in extreme flood frequency during the termination of the Little Ice Age (1830–1870 CE) and mid to late 20th century, both periods of Rapid Climate Change (RCC). The significant increase in flood frequency observed during RCC suggests that a similar pattern could be expected in the near future with the ongoing global warming.

Original languageEnglish (US)
Article number106963
JournalQuaternary Science Reviews
Volume262
DOIs
StatePublished - Jun 15 2021

Bibliographical note

Funding Information:
This project has received funding from the European Union’s Horizon 2020 research and innovation programme under the Marie Sklodowska-Curie grant agreement Nº 796752 (FLOODARC). Additional support has been obtained by the Spanish Ministry of Science, Innovation and Universities (MICINN) projects LIMNOCAL ( CGL 2006–13327. C04-01/CLI ), MEDLANT ( CGL2016-76215-R ), MEROMONT ( CGL2017-85682-R ) and EPHIMED ( CGL2017-86839-C3-1-R ) (co-financed with European FEDER funds). The Basque Water Agency facilitated access to its hydrological data.

Funding Information:
This project has received funding from the European Union's Horizon 2020 research and innovation programme under the Marie Sklodowska-Curie grant agreement N? 796752 (FLOODARC). Additional support has been obtained by the Spanish Ministry of Science, Innovation and Universities (MICINN) projects LIMNOCAL (CGL 2006?13327. C04-01/CLI), MEDLANT (CGL2016-76215-R), MEROMONT (CGL2017-85682-R) and EPHIMED (CGL2017-86839-C3-1-R) (co-financed with European FEDER funds). The Basque Water Agency facilitated access to its hydrological data.

Publisher Copyright:
© 2021 The Author(s)

Keywords

  • Historical floods
  • Lake
  • Late Holocene
  • Multi-archive integration
  • Paleofloods

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