Modelling of estuarine response to sea-level rise during the Holocene: Application to the Guadiana Estuary-SW Iberia

Detalhes bibliográficos
Autor(a) principal: Sampath, DMR
Data de Publicação: 2015
Outros Autores: Boski, T., Loureiro, Carlos, Sousa, Carlos A. Mendes da Silva de
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
Texto Completo: http://hdl.handle.net/10400.1/11639
Resumo: This paper focuses on simulations of the morphological evolution of an estuary during sedimentary infilling that accompanied Holocene sea-level rise. The simulations were conducted using the Estuarine Sedimentation Model, which uses a behaviour-oriented approach, supported by the chronostratigraphy of the estuary's sedimentary sequence. Behaviour curves were computed to represent the relationship between the estuarine channel depth below maximum high tide and the net accretion at a given location relative to the average sedimentation rate of the estuary during the Holocene. The model was validated by comparing the observed present-day bathymetry of the Guadiana River Estuary, southeastern Portugal, with the corresponding simulated bathymetries for nine control sections across the estuary. The best fit between simulated and actual sediment surface elevations was obtained along the cross-sections in the sheltered, low-energy environments of the estuary. The accuracy of the sedimentary stratigraphy of the best-fit model was further established using 16 radiocarbon ages obtained from five boreholes in the estuary. The present approach is particularly suitable for simulating long-term morphological evolution in sheltered estuarine environments where tidally driven vertical aggradation dominates at centennial to millennium timescales. However, the accuracy of simulated sediment surface elevations and consequently the robustness of behaviour-type models based on Geographical Information System platforms can be enhanced by incorporating (i) the impacts of nearshore hydrodynamic processes and episodic flood events in highly energetic channels, and (ii) the impacts of cross-currents in meandering channel sections. (C) 2015 Elsevier B.V. All rights reserved.
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spelling Modelling of estuarine response to sea-level rise during the Holocene: Application to the Guadiana Estuary-SW IberiaSediment Accumulation RatesDigital Elevation ModelsMorphological ResponseBathymetric EvolutionOsl ChronologyBound EstuarySalt-MarshPortugalStratigraphyClimateThis paper focuses on simulations of the morphological evolution of an estuary during sedimentary infilling that accompanied Holocene sea-level rise. The simulations were conducted using the Estuarine Sedimentation Model, which uses a behaviour-oriented approach, supported by the chronostratigraphy of the estuary's sedimentary sequence. Behaviour curves were computed to represent the relationship between the estuarine channel depth below maximum high tide and the net accretion at a given location relative to the average sedimentation rate of the estuary during the Holocene. The model was validated by comparing the observed present-day bathymetry of the Guadiana River Estuary, southeastern Portugal, with the corresponding simulated bathymetries for nine control sections across the estuary. The best fit between simulated and actual sediment surface elevations was obtained along the cross-sections in the sheltered, low-energy environments of the estuary. The accuracy of the sedimentary stratigraphy of the best-fit model was further established using 16 radiocarbon ages obtained from five boreholes in the estuary. The present approach is particularly suitable for simulating long-term morphological evolution in sheltered estuarine environments where tidally driven vertical aggradation dominates at centennial to millennium timescales. However, the accuracy of simulated sediment surface elevations and consequently the robustness of behaviour-type models based on Geographical Information System platforms can be enhanced by incorporating (i) the impacts of nearshore hydrodynamic processes and episodic flood events in highly energetic channels, and (ii) the impacts of cross-currents in meandering channel sections. (C) 2015 Elsevier B.V. All rights reserved.FCT [SFRH/BD/70747/2010, SFRH/BPD/85335/2012]Elsevier Science BvSapientiaSampath, DMRBoski, T.Loureiro, CarlosSousa, Carlos A. Mendes da Silva de2018-12-07T14:53:41Z2015-032015-03-01T00:00:00Zinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10400.1/11639eng0169-555X10.1016/j.geomorph.2014.12.037info:eu-repo/semantics/openAccessreponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãoinstacron:RCAAP2023-07-24T10:23:29Zoai:sapientia.ualg.pt:10400.1/11639Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireopendoar:71602024-03-19T20:03:07.149337Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãofalse
dc.title.none.fl_str_mv Modelling of estuarine response to sea-level rise during the Holocene: Application to the Guadiana Estuary-SW Iberia
title Modelling of estuarine response to sea-level rise during the Holocene: Application to the Guadiana Estuary-SW Iberia
spellingShingle Modelling of estuarine response to sea-level rise during the Holocene: Application to the Guadiana Estuary-SW Iberia
Sampath, DMR
Sediment Accumulation Rates
Digital Elevation Models
Morphological Response
Bathymetric Evolution
Osl Chronology
Bound Estuary
Salt-Marsh
Portugal
Stratigraphy
Climate
title_short Modelling of estuarine response to sea-level rise during the Holocene: Application to the Guadiana Estuary-SW Iberia
title_full Modelling of estuarine response to sea-level rise during the Holocene: Application to the Guadiana Estuary-SW Iberia
title_fullStr Modelling of estuarine response to sea-level rise during the Holocene: Application to the Guadiana Estuary-SW Iberia
title_full_unstemmed Modelling of estuarine response to sea-level rise during the Holocene: Application to the Guadiana Estuary-SW Iberia
title_sort Modelling of estuarine response to sea-level rise during the Holocene: Application to the Guadiana Estuary-SW Iberia
author Sampath, DMR
author_facet Sampath, DMR
Boski, T.
Loureiro, Carlos
Sousa, Carlos A. Mendes da Silva de
author_role author
author2 Boski, T.
Loureiro, Carlos
Sousa, Carlos A. Mendes da Silva de
author2_role author
author
author
dc.contributor.none.fl_str_mv Sapientia
dc.contributor.author.fl_str_mv Sampath, DMR
Boski, T.
Loureiro, Carlos
Sousa, Carlos A. Mendes da Silva de
dc.subject.por.fl_str_mv Sediment Accumulation Rates
Digital Elevation Models
Morphological Response
Bathymetric Evolution
Osl Chronology
Bound Estuary
Salt-Marsh
Portugal
Stratigraphy
Climate
topic Sediment Accumulation Rates
Digital Elevation Models
Morphological Response
Bathymetric Evolution
Osl Chronology
Bound Estuary
Salt-Marsh
Portugal
Stratigraphy
Climate
description This paper focuses on simulations of the morphological evolution of an estuary during sedimentary infilling that accompanied Holocene sea-level rise. The simulations were conducted using the Estuarine Sedimentation Model, which uses a behaviour-oriented approach, supported by the chronostratigraphy of the estuary's sedimentary sequence. Behaviour curves were computed to represent the relationship between the estuarine channel depth below maximum high tide and the net accretion at a given location relative to the average sedimentation rate of the estuary during the Holocene. The model was validated by comparing the observed present-day bathymetry of the Guadiana River Estuary, southeastern Portugal, with the corresponding simulated bathymetries for nine control sections across the estuary. The best fit between simulated and actual sediment surface elevations was obtained along the cross-sections in the sheltered, low-energy environments of the estuary. The accuracy of the sedimentary stratigraphy of the best-fit model was further established using 16 radiocarbon ages obtained from five boreholes in the estuary. The present approach is particularly suitable for simulating long-term morphological evolution in sheltered estuarine environments where tidally driven vertical aggradation dominates at centennial to millennium timescales. However, the accuracy of simulated sediment surface elevations and consequently the robustness of behaviour-type models based on Geographical Information System platforms can be enhanced by incorporating (i) the impacts of nearshore hydrodynamic processes and episodic flood events in highly energetic channels, and (ii) the impacts of cross-currents in meandering channel sections. (C) 2015 Elsevier B.V. All rights reserved.
publishDate 2015
dc.date.none.fl_str_mv 2015-03
2015-03-01T00:00:00Z
2018-12-07T14:53:41Z
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv http://hdl.handle.net/10400.1/11639
url http://hdl.handle.net/10400.1/11639
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv 0169-555X
10.1016/j.geomorph.2014.12.037
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv Elsevier Science Bv
publisher.none.fl_str_mv Elsevier Science Bv
dc.source.none.fl_str_mv reponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação
instacron:RCAAP
instname_str Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação
instacron_str RCAAP
institution RCAAP
reponame_str Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
collection Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
repository.name.fl_str_mv Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informação
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