Major coastal impact induced by a 1000-year storm event

Mikkel Fruergaard; Thorbjørn Joest Andersen; Peter Johannessen; Lars H. Nielsen; Morten Pejrup

doi:10.1038/srep01051

Major coastal impact induced by a 1000-year storm event

Mikkel Fruergaard, Thorbjørn Joest Andersen, Peter Johannessen, Lars H. Nielsen, Morten Pejrup

LUKKET: Geografi

39 Citationer (Scopus)

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Abstract

Extreme storms and storm surges may induce major changes along sandy barrier coastlines, potentially causing substantial environmental and economic damage. We show that the most destructive storm (the 1634 AD storm) documented for the northern Wadden Sea within the last thousand years both caused permanent barrier breaching and initiated accumulation of up to several metres of marine sand. An aggradational storm shoal and a prograding shoreface sand unit having thicknesses of up to 8 m and 5 m respectively were deposited as a result of the storm and during the subsequent 30 to 40 years long healing phase, on the eroded shoreface. Our results demonstrate that millennial-scale storms can induce large-scale and long-term changes on barrier coastlines and shorefaces, and that coastal changes assumed to take place over centuries or even millennia may occur in association with and be triggered by a single extreme storm event.

Originalsprog	Engelsk
Artikelnummer	1051
Tidsskrift	Scientific Reports
Vol/bind	3
Antal sider	7
ISSN	2045-2322
DOI	https://doi.org/10.1038/srep01051
Status	Udgivet - 2013

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Superstorme kan ramme Danmark: Superstorme som Sandy er ikke kun forbeholdt fremmede egne. En gigantisk storm ramte Danmark i 1634
Fruergaard, M.
03/03/2013
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Presse/medie

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abstract = "Extreme storms and storm surges may induce major changes along sandy barrier coastlines, potentially causing substantial environmental and economic damage. We show that the most destructive storm (the 1634 AD storm) documented for the northern Wadden Sea within the last thousand years both caused permanent barrier breaching and initiated accumulation of up to several metres of marine sand. An aggradational storm shoal and a prograding shoreface sand unit having thicknesses of up to 8 m and 5 m respectively were deposited as a result of the storm and during the subsequent 30 to 40 years long healing phase, on the eroded shoreface. Our results demonstrate that millennial-scale storms can induce large-scale and long-term changes on barrier coastlines and shorefaces, and that coastal changes assumed to take place over centuries or even millennia may occur in association with and be triggered by a single extreme storm event.",

author = "Mikkel Fruergaard and Andersen, {Thorbj{\o}rn Joest} and Peter Johannessen and Nielsen, {Lars H.} and Morten Pejrup",

year = "2013",

doi = "10.1038/srep01051",

language = "English",

volume = "3",

journal = "Scientific Reports",

issn = "2045-2322",

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TY - JOUR

T1 - Major coastal impact induced by a 1000-year storm event

AU - Fruergaard, Mikkel

AU - Andersen, Thorbjørn Joest

AU - Johannessen, Peter

AU - Nielsen, Lars H.

AU - Pejrup, Morten

PY - 2013

Y1 - 2013

N2 - Extreme storms and storm surges may induce major changes along sandy barrier coastlines, potentially causing substantial environmental and economic damage. We show that the most destructive storm (the 1634 AD storm) documented for the northern Wadden Sea within the last thousand years both caused permanent barrier breaching and initiated accumulation of up to several metres of marine sand. An aggradational storm shoal and a prograding shoreface sand unit having thicknesses of up to 8 m and 5 m respectively were deposited as a result of the storm and during the subsequent 30 to 40 years long healing phase, on the eroded shoreface. Our results demonstrate that millennial-scale storms can induce large-scale and long-term changes on barrier coastlines and shorefaces, and that coastal changes assumed to take place over centuries or even millennia may occur in association with and be triggered by a single extreme storm event.

AB - Extreme storms and storm surges may induce major changes along sandy barrier coastlines, potentially causing substantial environmental and economic damage. We show that the most destructive storm (the 1634 AD storm) documented for the northern Wadden Sea within the last thousand years both caused permanent barrier breaching and initiated accumulation of up to several metres of marine sand. An aggradational storm shoal and a prograding shoreface sand unit having thicknesses of up to 8 m and 5 m respectively were deposited as a result of the storm and during the subsequent 30 to 40 years long healing phase, on the eroded shoreface. Our results demonstrate that millennial-scale storms can induce large-scale and long-term changes on barrier coastlines and shorefaces, and that coastal changes assumed to take place over centuries or even millennia may occur in association with and be triggered by a single extreme storm event.

U2 - 10.1038/srep01051

DO - 10.1038/srep01051

M3 - Journal article

SN - 2045-2322

VL - 3

JO - Scientific Reports

JF - Scientific Reports

M1 - 1051

ER -

Major coastal impact induced by a 1000-year storm event

Abstract

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Superstorme kan ramme Danmark: Superstorme som Sandy er ikke kun forbeholdt fremmede egne. En gigantisk storm ramte Danmark i 1634

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