The significance of coastal bathymetry representation for modelling the tidal response to mean sea level rise in the German Bight

<p>Due to climate change an accelerated mean sea level rise is expected. One key question for the development of adaptation measures is how mean sea level rise affects tidal dynamics in shelf seas such as the North Sea. Owing to its low-lying coastal areas, the German Bight (located in the sou...

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Main Authors: C. Rasquin, R. Seiffert, B. Wachler, N. Winkel
Format: Article
Language:English
Published: Copernicus Publications 2020-01-01
Series:Ocean Science
Online Access:https://www.ocean-sci.net/16/31/2020/os-16-31-2020.pdf
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spelling doaj-883fff4fa97f4cc6ab13733fe03a81c72020-11-25T02:43:16ZengCopernicus PublicationsOcean Science1812-07841812-07922020-01-0116314410.5194/os-16-31-2020The significance of coastal bathymetry representation for modelling the tidal response to mean sea level rise in the German BightC. RasquinR. SeiffertB. WachlerN. Winkel<p>Due to climate change an accelerated mean sea level rise is expected. One key question for the development of adaptation measures is how mean sea level rise affects tidal dynamics in shelf seas such as the North Sea. Owing to its low-lying coastal areas, the German Bight (located in the southeast of the North Sea) will be especially affected. Numerical hydrodynamic models help to understand how mean sea level rise changes tidal dynamics. Models cannot adequately represent all processes in overall detail. One limiting factor is the resolution of the model grid. In this study we investigate which role the representation of the coastal bathymetry plays when analysing the response of tidal dynamics to mean sea level rise.</p> <p>Using a shelf model including the whole North Sea and a high-resolution hydrodynamic model of the German Bight we investigate the changes in M2 amplitude due to a mean sea level rise of 0.8 and 10&thinsp;m. The shelf model and the German Bight Model react in different ways. In the simulations with a mean sea level rise of 0.8&thinsp;m the M2 amplitude in the shelf model generally increases in the region of the German Bight. In contrast, the M2 amplitude in the German Bight Model increases only in some coastal areas and decreases in the northern part of the German Bight. In the simulations with a mean sea level rise of 10&thinsp;m the M2 amplitude increases in both models with largely similar spatial patterns. In two case studies we adjust the German Bight Model in order to more closely resemble the shelf model. We find that a different resolution of the bathymetry results in different energy dissipation changes in response to mean sea level rise. Our results show that the resolution of the bathymetry especially in flat intertidal areas plays a crucial role for modelling the impact of mean sea level rise.</p>https://www.ocean-sci.net/16/31/2020/os-16-31-2020.pdf
collection DOAJ
language English
format Article
sources DOAJ
author C. Rasquin
R. Seiffert
B. Wachler
N. Winkel
spellingShingle C. Rasquin
R. Seiffert
B. Wachler
N. Winkel
The significance of coastal bathymetry representation for modelling the tidal response to mean sea level rise in the German Bight
Ocean Science
author_facet C. Rasquin
R. Seiffert
B. Wachler
N. Winkel
author_sort C. Rasquin
title The significance of coastal bathymetry representation for modelling the tidal response to mean sea level rise in the German Bight
title_short The significance of coastal bathymetry representation for modelling the tidal response to mean sea level rise in the German Bight
title_full The significance of coastal bathymetry representation for modelling the tidal response to mean sea level rise in the German Bight
title_fullStr The significance of coastal bathymetry representation for modelling the tidal response to mean sea level rise in the German Bight
title_full_unstemmed The significance of coastal bathymetry representation for modelling the tidal response to mean sea level rise in the German Bight
title_sort significance of coastal bathymetry representation for modelling the tidal response to mean sea level rise in the german bight
publisher Copernicus Publications
series Ocean Science
issn 1812-0784
1812-0792
publishDate 2020-01-01
description <p>Due to climate change an accelerated mean sea level rise is expected. One key question for the development of adaptation measures is how mean sea level rise affects tidal dynamics in shelf seas such as the North Sea. Owing to its low-lying coastal areas, the German Bight (located in the southeast of the North Sea) will be especially affected. Numerical hydrodynamic models help to understand how mean sea level rise changes tidal dynamics. Models cannot adequately represent all processes in overall detail. One limiting factor is the resolution of the model grid. In this study we investigate which role the representation of the coastal bathymetry plays when analysing the response of tidal dynamics to mean sea level rise.</p> <p>Using a shelf model including the whole North Sea and a high-resolution hydrodynamic model of the German Bight we investigate the changes in M2 amplitude due to a mean sea level rise of 0.8 and 10&thinsp;m. The shelf model and the German Bight Model react in different ways. In the simulations with a mean sea level rise of 0.8&thinsp;m the M2 amplitude in the shelf model generally increases in the region of the German Bight. In contrast, the M2 amplitude in the German Bight Model increases only in some coastal areas and decreases in the northern part of the German Bight. In the simulations with a mean sea level rise of 10&thinsp;m the M2 amplitude increases in both models with largely similar spatial patterns. In two case studies we adjust the German Bight Model in order to more closely resemble the shelf model. We find that a different resolution of the bathymetry results in different energy dissipation changes in response to mean sea level rise. Our results show that the resolution of the bathymetry especially in flat intertidal areas plays a crucial role for modelling the impact of mean sea level rise.</p>
url https://www.ocean-sci.net/16/31/2020/os-16-31-2020.pdf
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