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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| Hauptverfasser: | , , , , , , , , , , |
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| Dokumenttyp: | Article (Journal) |
| Sprache: | Englisch |
| Veröffentlicht: |
2024
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| In: |
Journal of quaternary science
Year: 2024, Jahrgang: 39, Heft: 1, Pages: 37-53 |
| ISSN: | 1099-1417 |
| DOI: | 10.1002/jqs.3568 |
| Online-Zugang: | Verlag, kostenfrei, Volltext: https://doi.org/10.1002/jqs.3568 Verlag, kostenfrei, Volltext: https://onlinelibrary.wiley.com/doi/abs/10.1002/jqs.3568 
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| Verfasserangaben: | Katharina Hess, Max Engel, Tasnim Patel, Polina Vakhrameeva, Andreas Koutsodendris, Eckehard Klemt, Thor H. Hansteen, Philipp Kempf, Sue Dawson, Isa Schön and Vanessa M. A. Heyvaert |
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| 245 | 1 | 2 | |a A 1500-year record of North Atlantic storm flooding from lacustrine sediments, Shetland Islands (UK) |c Katharina Hess, Max Engel, Tasnim Patel, Polina Vakhrameeva, Andreas Koutsodendris, Eckehard Klemt, Thor H. Hansteen, Philipp Kempf, Sue Dawson, Isa Schön and Vanessa M. A. Heyvaert |
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| 520 | |a 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 14C and 137Cs 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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| 650 | 4 | |a storm frequency | |
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