Simulating Destructive and Constructive Morphodynamic Processes in Steep Beaches

Short-term beach morphodynamics are typically modelled solely through storm-induced erosion, disregarding post-storm recovery. Yet, the full cycle of beach profile response is critical to simulating and understanding morphodynamics over longer temporal scales. The XBeach model is calibrated using to...

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Main Authors: Katerina Kombiadou, Susana Costas, Dano Roelvink
Format: Article
Language:English
Published: MDPI AG 2021-01-01
Series:Journal of Marine Science and Engineering
Subjects:
Online Access:https://www.mdpi.com/2077-1312/9/1/86
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spelling doaj-aaa32fc522d04b0ba066ef013d8ba1af2021-04-02T19:46:08ZengMDPI AGJournal of Marine Science and Engineering2077-13122021-01-019868610.3390/jmse9010086Simulating Destructive and Constructive Morphodynamic Processes in Steep BeachesKaterina Kombiadou0Susana Costas1Dano Roelvink2CIMA–Centre for Marine and Environmental Research, FCT, Campus de Gambelas, Universidade do Algarve, 8005-139 Faro, PortugalCIMA–Centre for Marine and Environmental Research, FCT, Campus de Gambelas, Universidade do Algarve, 8005-139 Faro, PortugalWater Science and Engineering Department, IHE Delft institute for Water Education, Westvest 7, 2611 AX Delft, The NetherlandsShort-term beach morphodynamics are typically modelled solely through storm-induced erosion, disregarding post-storm recovery. Yet, the full cycle of beach profile response is critical to simulating and understanding morphodynamics over longer temporal scales. The XBeach model is calibrated using topographic profiles from a reflective beach (Faro Beach, in S. Portugal) during and after the incidence of a fierce storm (Emma) that impacted the area in early 2018. Recovery in all three profiles showed rapid steepening of the beachface and significant recovery of eroded volumes (68–92%) within 45 days after the storm, while berm heights reached 4.5–5 m. Two calibration parameters were used (<i>facua</i> and <i>bermslope</i>), considering two sets of values, one for erosive (Hm0 ≥ 3 m) and one for accretive (Hm0 < 3 m) conditions. A correction of the runup height underestimation by the model in surfbeat mode was necessary to reproduce the measured berm elevation and morphology during recovery. Simulated profiles effectively capture storm erosion, but also berm growth and gradual recovery of the profiles, showing good skill in all three profiles and recovery phases. These experiments will be the basis to formulate event-scale simulations using schematized wave forcing that will allow to calibrate the model for longer-term changes.https://www.mdpi.com/2077-1312/9/1/86morphodynamic modellingbeach recoveryXBeachsurfbeatbermbermslope
collection DOAJ
language English
format Article
sources DOAJ
author Katerina Kombiadou
Susana Costas
Dano Roelvink
spellingShingle Katerina Kombiadou
Susana Costas
Dano Roelvink
Simulating Destructive and Constructive Morphodynamic Processes in Steep Beaches
Journal of Marine Science and Engineering
morphodynamic modelling
beach recovery
XBeach
surfbeat
berm
bermslope
author_facet Katerina Kombiadou
Susana Costas
Dano Roelvink
author_sort Katerina Kombiadou
title Simulating Destructive and Constructive Morphodynamic Processes in Steep Beaches
title_short Simulating Destructive and Constructive Morphodynamic Processes in Steep Beaches
title_full Simulating Destructive and Constructive Morphodynamic Processes in Steep Beaches
title_fullStr Simulating Destructive and Constructive Morphodynamic Processes in Steep Beaches
title_full_unstemmed Simulating Destructive and Constructive Morphodynamic Processes in Steep Beaches
title_sort simulating destructive and constructive morphodynamic processes in steep beaches
publisher MDPI AG
series Journal of Marine Science and Engineering
issn 2077-1312
publishDate 2021-01-01
description Short-term beach morphodynamics are typically modelled solely through storm-induced erosion, disregarding post-storm recovery. Yet, the full cycle of beach profile response is critical to simulating and understanding morphodynamics over longer temporal scales. The XBeach model is calibrated using topographic profiles from a reflective beach (Faro Beach, in S. Portugal) during and after the incidence of a fierce storm (Emma) that impacted the area in early 2018. Recovery in all three profiles showed rapid steepening of the beachface and significant recovery of eroded volumes (68–92%) within 45 days after the storm, while berm heights reached 4.5–5 m. Two calibration parameters were used (<i>facua</i> and <i>bermslope</i>), considering two sets of values, one for erosive (Hm0 ≥ 3 m) and one for accretive (Hm0 < 3 m) conditions. A correction of the runup height underestimation by the model in surfbeat mode was necessary to reproduce the measured berm elevation and morphology during recovery. Simulated profiles effectively capture storm erosion, but also berm growth and gradual recovery of the profiles, showing good skill in all three profiles and recovery phases. These experiments will be the basis to formulate event-scale simulations using schematized wave forcing that will allow to calibrate the model for longer-term changes.
topic morphodynamic modelling
beach recovery
XBeach
surfbeat
berm
bermslope
url https://www.mdpi.com/2077-1312/9/1/86
work_keys_str_mv AT katerinakombiadou simulatingdestructiveandconstructivemorphodynamicprocessesinsteepbeaches
AT susanacostas simulatingdestructiveandconstructivemorphodynamicprocessesinsteepbeaches
AT danoroelvink simulatingdestructiveandconstructivemorphodynamicprocessesinsteepbeaches
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