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North Sea storminess from a novel storm surge record since AD 1843*

North Sea storminess from a novel storm surge record since AD 1843*
North Sea storminess from a novel storm surge record since AD 1843*
The detection of potential long-term changes in historical storm statistics and storm surges plays a vitally important role for protecting coastal communities. In the absence of long homogeneous wind records, the authors present a novel, independent, and homogeneous storm surge record based on water level observations in the North Sea since 1843. Storm surges are characterized by considerable interannual-to-decadal variability linked to large-scale atmospheric circulation patterns. Time periods of increased storm surge levels prevailed in the late nineteenth and twentieth centuries without any evidence for significant long-term trends. This contradicts with recent findings based on reanalysis data, which suggest increasing storminess in the region since the late nineteenth century. The authors compare the wind and pressure fields from the Twentieth-Century Reanalysis (20CRv2) with the storm surge record by applying state-of-the-art empirical wind surge formulas. The comparison reveals that the reanalysis is a valuable tool that leads to good results over the past 100 yr; previously the statistical relationship fails, leaving significantly lower values in the upper percentiles of the predicted surge time series. These low values lead to significant upward trends over the entire investigation period, which are in turn supported by neither the storm surge record nor an independent circulation index based on homogeneous pressure readings. The authors therefore suggest that these differences are related to higher uncertainties in the earlier years of the 20CRv2 over the North Sea region.
0894-8755
3582-3595
Dangendorf, Sönke
ba1c5cbe-a385-41dc-8a46-da8cd36cf19d
Müller-Navarra, Sylvin
f0241c2a-88ee-48e6-8cae-3349eab36f50
Jensen, Jürgen
5188f969-c5e8-47e2-9e27-771067712095
Schenk, Frederik
52c04f57-f216-4d09-a56c-63924cf399b1
Wahl, Thomas
6506794a-1f35-4803-b7f7-98702e57e667
Weisse, Ralf
85957432-111d-407c-8551-7083092ce18d
Dangendorf, Sönke
ba1c5cbe-a385-41dc-8a46-da8cd36cf19d
Müller-Navarra, Sylvin
f0241c2a-88ee-48e6-8cae-3349eab36f50
Jensen, Jürgen
5188f969-c5e8-47e2-9e27-771067712095
Schenk, Frederik
52c04f57-f216-4d09-a56c-63924cf399b1
Wahl, Thomas
6506794a-1f35-4803-b7f7-98702e57e667
Weisse, Ralf
85957432-111d-407c-8551-7083092ce18d

Dangendorf, Sönke, Müller-Navarra, Sylvin, Jensen, Jürgen, Schenk, Frederik, Wahl, Thomas and Weisse, Ralf (2014) North Sea storminess from a novel storm surge record since AD 1843*. Journal of Climate, 27 (10), 3582-3595. (doi:10.1175/JCLI-D-13-00427.1).

Record type: Article

Abstract

The detection of potential long-term changes in historical storm statistics and storm surges plays a vitally important role for protecting coastal communities. In the absence of long homogeneous wind records, the authors present a novel, independent, and homogeneous storm surge record based on water level observations in the North Sea since 1843. Storm surges are characterized by considerable interannual-to-decadal variability linked to large-scale atmospheric circulation patterns. Time periods of increased storm surge levels prevailed in the late nineteenth and twentieth centuries without any evidence for significant long-term trends. This contradicts with recent findings based on reanalysis data, which suggest increasing storminess in the region since the late nineteenth century. The authors compare the wind and pressure fields from the Twentieth-Century Reanalysis (20CRv2) with the storm surge record by applying state-of-the-art empirical wind surge formulas. The comparison reveals that the reanalysis is a valuable tool that leads to good results over the past 100 yr; previously the statistical relationship fails, leaving significantly lower values in the upper percentiles of the predicted surge time series. These low values lead to significant upward trends over the entire investigation period, which are in turn supported by neither the storm surge record nor an independent circulation index based on homogeneous pressure readings. The authors therefore suggest that these differences are related to higher uncertainties in the earlier years of the 20CRv2 over the North Sea region.

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More information

Accepted/In Press date: 6 January 2014
Published date: 9 May 2014
Organisations: Energy & Climate Change Group

Identifiers

Local EPrints ID: 393894
URI: http://eprints.soton.ac.uk/id/eprint/393894
ISSN: 0894-8755
PURE UUID: ea08bb4d-afa7-415a-91ff-c199d75f1955

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Date deposited: 09 May 2016 10:48
Last modified: 15 Mar 2024 00:12

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Contributors

Author: Sönke Dangendorf
Author: Sylvin Müller-Navarra
Author: Jürgen Jensen
Author: Frederik Schenk
Author: Thomas Wahl
Author: Ralf Weisse

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