The role of morphodynamics in predicting coastal flooding from storms on a dissipative beach with sea level rise conditions

We investigate the role of morphodynamic changes in the flooding of a micro-tidal dissipative beach for both current and sea level rise scenarios. By considering beach morphodynamics and flood processes associated with highly energetic waves, the study allows one to evaluate threats to coastal zones...

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Autores:
Cueto, Jairo
Otero Díaz, Luis J.
Ospino Ortiz, Silvio Raul
Torres-Freyermuth, Alec
Tipo de recurso:
Article of journal
Fecha de publicación:
2022
Institución:
Corporación Universidad de la Costa
Repositorio:
REDICUC - Repositorio CUC
Idioma:
eng
OAI Identifier:
oai:repositorio.cuc.edu.co:11323/9169
Acceso en línea:
https://hdl.handle.net/11323/9169
https://repositorio.cuc.edu.co/
Palabra clave:
Coastal flooding
Sea ​​levels
Morphodynamic
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openAccess
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© Author(s) 2022. This work is distributed under the Creative Commons Attribution 4.0 License.
id RCUC2_b8e6ec33ca8cec6a812348866a7e6058
oai_identifier_str oai:repositorio.cuc.edu.co:11323/9169
network_acronym_str RCUC2
network_name_str REDICUC - Repositorio CUC
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dc.title.eng.fl_str_mv The role of morphodynamics in predicting coastal flooding from storms on a dissipative beach with sea level rise conditions
title The role of morphodynamics in predicting coastal flooding from storms on a dissipative beach with sea level rise conditions
spellingShingle The role of morphodynamics in predicting coastal flooding from storms on a dissipative beach with sea level rise conditions
Coastal flooding
Sea ​​levels
Morphodynamic
title_short The role of morphodynamics in predicting coastal flooding from storms on a dissipative beach with sea level rise conditions
title_full The role of morphodynamics in predicting coastal flooding from storms on a dissipative beach with sea level rise conditions
title_fullStr The role of morphodynamics in predicting coastal flooding from storms on a dissipative beach with sea level rise conditions
title_full_unstemmed The role of morphodynamics in predicting coastal flooding from storms on a dissipative beach with sea level rise conditions
title_sort The role of morphodynamics in predicting coastal flooding from storms on a dissipative beach with sea level rise conditions
dc.creator.fl_str_mv Cueto, Jairo
Otero Díaz, Luis J.
Ospino Ortiz, Silvio Raul
Torres-Freyermuth, Alec
dc.contributor.author.spa.fl_str_mv Cueto, Jairo
Otero Díaz, Luis J.
Ospino Ortiz, Silvio Raul
Torres-Freyermuth, Alec
dc.subject.proposal.eng.fl_str_mv Coastal flooding
Sea ​​levels
Morphodynamic
topic Coastal flooding
Sea ​​levels
Morphodynamic
description We investigate the role of morphodynamic changes in the flooding of a micro-tidal dissipative beach for both current and sea level rise scenarios. By considering beach morphodynamics and flood processes associated with highly energetic waves, the study allows one to evaluate threats to coastal zones. Coupling of SWAN and XBeach models is employed to propagate offshore wave conditions to the swash zone, estimating morphological changes and flooding associated with wave conditions during cold fronts and hurricanes that affected Cartagena de Indias (Colombia). The numerical models were calibrated from previous research in the study area. The results indicate that numerical modeling of flooding on microtidal dissipative beaches under extreme wave conditions should be approached by considering beach morphodynamics, because ignoring them can underestimate flooding by ∼ 15 %. Moreover, model results suggest that beach erosion and flooding are intensified by sea level rise, resulting in the most unfavorable condition when extreme events are contemporaneous with high tides. In this case, the increase in erosion and flooding is ∼ 69 % and ∼ 65 %, respectively, when compared with the present conditions of sea level.
publishDate 2022
dc.date.accessioned.none.fl_str_mv 2022-05-17T15:47:59Z
dc.date.available.none.fl_str_mv 2022-05-17T15:47:59Z
dc.date.issued.none.fl_str_mv 2022
dc.type.spa.fl_str_mv Artículo de revista
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dc.type.coar.spa.fl_str_mv http://purl.org/coar/resource_type/c_6501
dc.type.content.spa.fl_str_mv Text
dc.type.driver.spa.fl_str_mv info:eu-repo/semantics/article
dc.type.redcol.spa.fl_str_mv http://purl.org/redcol/resource_type/ART
dc.type.version.spa.fl_str_mv info:eu-repo/semantics/acceptedVersion
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dc.identifier.citation.spa.fl_str_mv Cueto, J. E., Otero Díaz, L. J., Ospino-Ortiz, S. R., and Torres-Freyermuth, A.: The role of morphodynamics in predicting coastal flooding from storms on a dissipative beach with sea level rise conditions, Nat. Hazards Earth Syst. Sci., 22, 713–728, https://doi.org/10.5194/nhess-22-713-2022, 2022.
dc.identifier.issn.spa.fl_str_mv 1561-8633
dc.identifier.uri.spa.fl_str_mv https://hdl.handle.net/11323/9169
dc.identifier.doi.spa.fl_str_mv 10.5194/nhess-22-713-2022, 2022.
dc.identifier.eissn.spa.fl_str_mv 1684-9981
dc.identifier.instname.spa.fl_str_mv Corporación Universidad de la Costa
dc.identifier.reponame.spa.fl_str_mv REDICUC - Repositorio CUC
dc.identifier.repourl.spa.fl_str_mv https://repositorio.cuc.edu.co/
identifier_str_mv Cueto, J. E., Otero Díaz, L. J., Ospino-Ortiz, S. R., and Torres-Freyermuth, A.: The role of morphodynamics in predicting coastal flooding from storms on a dissipative beach with sea level rise conditions, Nat. Hazards Earth Syst. Sci., 22, 713–728, https://doi.org/10.5194/nhess-22-713-2022, 2022.
1561-8633
10.5194/nhess-22-713-2022, 2022.
1684-9981
Corporación Universidad de la Costa
REDICUC - Repositorio CUC
url https://hdl.handle.net/11323/9169
https://repositorio.cuc.edu.co/
dc.language.iso.none.fl_str_mv eng
language eng
dc.relation.ispartofjournal.spa.fl_str_mv Natural Hazards and Earth System Sciences
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spelling Cueto, JairoOtero Díaz, Luis J.Ospino Ortiz, Silvio RaulTorres-Freyermuth, Alec2022-05-17T15:47:59Z2022-05-17T15:47:59Z2022Cueto, J. E., Otero Díaz, L. J., Ospino-Ortiz, S. R., and Torres-Freyermuth, A.: The role of morphodynamics in predicting coastal flooding from storms on a dissipative beach with sea level rise conditions, Nat. Hazards Earth Syst. Sci., 22, 713–728, https://doi.org/10.5194/nhess-22-713-2022, 2022.1561-8633https://hdl.handle.net/11323/916910.5194/nhess-22-713-2022, 2022.1684-9981Corporación Universidad de la CostaREDICUC - Repositorio CUChttps://repositorio.cuc.edu.co/We investigate the role of morphodynamic changes in the flooding of a micro-tidal dissipative beach for both current and sea level rise scenarios. By considering beach morphodynamics and flood processes associated with highly energetic waves, the study allows one to evaluate threats to coastal zones. Coupling of SWAN and XBeach models is employed to propagate offshore wave conditions to the swash zone, estimating morphological changes and flooding associated with wave conditions during cold fronts and hurricanes that affected Cartagena de Indias (Colombia). The numerical models were calibrated from previous research in the study area. The results indicate that numerical modeling of flooding on microtidal dissipative beaches under extreme wave conditions should be approached by considering beach morphodynamics, because ignoring them can underestimate flooding by ∼ 15 %. Moreover, model results suggest that beach erosion and flooding are intensified by sea level rise, resulting in the most unfavorable condition when extreme events are contemporaneous with high tides. In this case, the increase in erosion and flooding is ∼ 69 % and ∼ 65 %, respectively, when compared with the present conditions of sea level.16 páginasapplication/pdfengEuropean Geosciences UnionGermany© Author(s) 2022. 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Eng., 137, 1549–1564, https://doi.org/10.1061/(ASCE)HY.1943-7900.0000498, 2011.728713322Coastal floodingSea ​​levelsMorphodynamicPublicationORIGINALThe role of morphodynamics in predicting coastal flooding from storms on a dissipative beach with sea level rise conditions.pdfThe role of morphodynamics in predicting coastal flooding from storms on a dissipative beach with sea level rise conditions.pdfapplication/pdf8355610https://repositorio.cuc.edu.co/bitstreams/b5b69db0-32d7-4cc7-b509-e9baef3ed8d6/download6ac484de0ec091f6643b9dbce60da0faMD51LICENSElicense.txtlicense.txttext/plain; charset=utf-83196https://repositorio.cuc.edu.co/bitstreams/79c31c90-673c-4396-98c3-40daa3ddac86/downloade30e9215131d99561d40d6b0abbe9badMD52TEXTThe role of morphodynamics in predicting coastal flooding from storms on a dissipative beach with sea level rise conditions.pdf.txtThe role of morphodynamics in predicting coastal flooding from storms on a dissipative beach with sea level rise conditions.pdf.txttext/plain66566https://repositorio.cuc.edu.co/bitstreams/44b69af5-558c-4ece-a279-f95ebbf3fa92/download3dcba38ee21dea9d731ee499c598990dMD53THUMBNAILThe role of morphodynamics in predicting coastal flooding from storms on a dissipative beach with sea level rise conditions.pdf.jpgThe role of morphodynamics in predicting coastal flooding from storms on a dissipative beach with sea level rise conditions.pdf.jpgimage/jpeg15593https://repositorio.cuc.edu.co/bitstreams/19ee9f03-bf13-463b-b8aa-8bdf783258b0/download67424e101216a410e1c38568587429deMD5411323/9169oai:repositorio.cuc.edu.co:11323/91692024-09-17 10:59:24.325https://creativecommons.org/licenses/by/4.0/© Author(s) 2022. This work is distributed under the Creative Commons Attribution 4.0 License.open.accesshttps://repositorio.cuc.edu.coRepositorio de la Universidad de la Costa CUCrepdigital@cuc.edu.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