A 1500‐year record of North Atlantic storm flooding from lacustrine sediments, Shetland Islands (UK)

Severe storm flooding poses a major hazard to the coasts of north‐western Europe. However, the long‐term recurrence patterns of extreme coastal flooding and their governing factors are poorly understood. Therefore, high‐resolution sedimentary records of past North Atlantic storm flooding are require...

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Bibliographic Details
Published in:Journal of Quaternary Science
Main Authors: Hess, Katharina, Engel, Max, Patel, Tasnim, Vakhrameeva, Polina, Koutsodendris, Andreas, Klemt, Eckehard, Hansteen, Thor H., Kempf, Philipp, Dawson, Sue, Schön, Isa, Heyvaert, Vanessa M. A.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2024
Subjects:
North Atlantic
North Atlantic oscillation
North East Atlantic
Online Access:https://oceanrep.geomar.de/id/eprint/59222/
https://oceanrep.geomar.de/id/eprint/59222/7/J%20Quaternary%20Science%20-%202023%20-%20Hess%20-%20A%201500%E2%80%90year%20record%20of%20North%20Atlantic%20storm%20flooding%20from%20lacustrine%20sediments%20.pdf
https://doi.org/10.1002/jqs.3568
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Summary:Severe storm flooding poses a major hazard to the coasts of north‐western Europe. However, the long‐term recurrence patterns of extreme coastal flooding and their governing factors are poorly understood. Therefore, high‐resolution sedimentary records of past North Atlantic storm flooding are required. This multi‐proxy study reconstructs storm‐induced overwash processes from coastal lake sediments on the Shetland Islands using grain‐size and geochemical data, and the re‐analysis of historical data. The chronostratigraphy is based on Bayesian age–depth modelling using accelerator mass spectrometry 14 C and 137 Cs data. A high XRF‐based Si/Ti ratio and the unimodal grain‐size distribution link the sand layers to the beach and thus storm‐induced overwash events. Periods with more frequent storm flooding occurred 980–1050, 1150–1300, 1450–1550, 1820–1900 and 1950–2000 ce, which is largely consistent with a positive North Atlantic Oscillation mode. The Little Ice Age (1400–1850 ce ) shows a gap of major sand layers suggesting a southward shift of storm tracks and a seasonal variance with more storm floods in spring and autumn. Warmer phases shifted winter storm tracks towards the north‐east Atlantic, indicating a possible trend for future storm‐track changes and increased storm flooding in the northern North Sea region.

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