The Coastline Evolution Model 2D (CEM2D) V1.1
<p>Coasts are among the most intensely used environments on the planet, but they also present dynamic and unique hazards, including flooding and erosion. Sea level rise and changing wave climates will alter patterns of erosion and deposition, but some existing coastline evolution models are un...
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Copernicus Publications
2021-09-01
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doaj-c11d8fb6cb824798a0c5ad45bcc63f3e2021-09-07T07:33:13ZengCopernicus PublicationsGeoscientific Model Development1991-959X1991-96032021-09-01145507552310.5194/gmd-14-5507-2021The Coastline Evolution Model 2D (CEM2D) V1.1C. Leach0T. Coulthard1A. Barkwith2D. R. Parsons3S. Manson4School of Geography, The University of Melbourne, Parkville, Melbourne, VIC 3010, AustraliaDepartment of Geography, Geology and Environmental Science, University of Hull, Hull, HU6 7RX, UKBritish Geological Survey, Environmental Science Centre, Keyworth, Nottingham, NG12 5GG, UKDepartment of Geography, Geology and Environmental Science, University of Hull, Hull, HU6 7RX, UKEnvironment Agency, Crosskill House, Mill Lane, Beverley, HU17 9JW, UK<p>Coasts are among the most intensely used environments on the planet, but they also present dynamic and unique hazards, including flooding and erosion. Sea level rise and changing wave climates will alter patterns of erosion and deposition, but some existing coastline evolution models are unable to simulate these effects due to their one-dimensional representation of the systems or the sediment transport processes. In this paper, the development and application of the Coastline Evolution Model 2D (CEM2D) are presented, a model which incorporates these influences. The model has been developed from the established CEM and is capable of simulating fundamental cause–effect relationships in coastal systems. The two-dimensional storage and transport of sediment in CEM2D, which are only done in one-dimension in CEM, mean it is also capable of exploring the influence of a variable water level on sediment transport and the formation and evolution of morphological features and landforms at the mesoscale. The model sits between one-dimensional and three-dimensional models, with the advantage of increased complexity and detail in model outputs compared to the former but with more efficiency and less computational expense than the latter.</p>https://gmd.copernicus.org/articles/14/5507/2021/gmd-14-5507-2021.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
C. Leach T. Coulthard A. Barkwith D. R. Parsons S. Manson |
spellingShingle |
C. Leach T. Coulthard A. Barkwith D. R. Parsons S. Manson The Coastline Evolution Model 2D (CEM2D) V1.1 Geoscientific Model Development |
author_facet |
C. Leach T. Coulthard A. Barkwith D. R. Parsons S. Manson |
author_sort |
C. Leach |
title |
The Coastline Evolution Model 2D (CEM2D) V1.1 |
title_short |
The Coastline Evolution Model 2D (CEM2D) V1.1 |
title_full |
The Coastline Evolution Model 2D (CEM2D) V1.1 |
title_fullStr |
The Coastline Evolution Model 2D (CEM2D) V1.1 |
title_full_unstemmed |
The Coastline Evolution Model 2D (CEM2D) V1.1 |
title_sort |
coastline evolution model 2d (cem2d) v1.1 |
publisher |
Copernicus Publications |
series |
Geoscientific Model Development |
issn |
1991-959X 1991-9603 |
publishDate |
2021-09-01 |
description |
<p>Coasts are among the most intensely used environments on
the planet, but they also present dynamic and unique hazards, including
flooding and erosion. Sea level rise and changing wave climates will alter
patterns of erosion and deposition, but some existing coastline evolution
models are unable to simulate these effects due to their one-dimensional
representation of the systems or the sediment transport processes. In this
paper, the development and application of the Coastline Evolution Model 2D
(CEM2D) are presented, a model which incorporates these influences. The model has
been developed from the established CEM and is capable of simulating
fundamental cause–effect relationships in coastal systems. The
two-dimensional storage and transport of sediment in CEM2D, which are only
done in one-dimension in CEM, mean it is also capable of exploring the
influence of a variable water level on sediment transport and the formation
and evolution of morphological features and landforms at the mesoscale. The
model sits between one-dimensional and three-dimensional models, with the
advantage of increased complexity and detail in model outputs compared to
the former but with more efficiency and less computational expense than the
latter.</p> |
url |
https://gmd.copernicus.org/articles/14/5507/2021/gmd-14-5507-2021.pdf |
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