Influence of the Barrie de la Maza dock on the circulation pattern of the Ría of a Coruña (NW-Spain)

Detalhes bibliográficos
Autor(a) principal: Gómez-Gesteira, Moncho
Data de Publicação: 2008
Outros Autores: Decastro, Maite, Prego, Ricardo, Martins, Flávio Augusto Bastos da Cruz
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
Texto Completo: http://hdl.handle.net/10400.1/168
Resumo: A 3D hydrodynamical model is applied to the ria of A Coruña to analyze the evolution of the circulation pattern in the ria after the building of a breakwater (Barrie de la Maza dock) in the sixties. This circulation pattern has changed greatly. On the one hand, the circulation, which was almost parallel to the shore line under the original conditions, now shows a gyre near the end of the dock. On the other hand, a considerable increase (about 30%) in the velocities near the end of the breakwater and in the main channel of the estuary has been observed after the building of the dock. A stronger bottom shear stress has been generated in the estuary areas where the velocity increased. The bottom shear stress increase was particularly great (over 100%) near the end of the dock. This increase in the shear stress produced bottom erosion and matter resuspension, and consequently major changes in the bathymetry. In addition, in situ sedimentary measurements carried out by Lopez-Jamar (1996) corroborate the bottom erosion in the main chanel of the estuary and at the end of the dock produced by the velocity increase generated by the building of the breakwater.
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spelling Influence of the Barrie de la Maza dock on the circulation pattern of the Ría of a Coruña (NW-Spain)EstuáriosQuebra mares532A 3D hydrodynamical model is applied to the ria of A Coruña to analyze the evolution of the circulation pattern in the ria after the building of a breakwater (Barrie de la Maza dock) in the sixties. This circulation pattern has changed greatly. On the one hand, the circulation, which was almost parallel to the shore line under the original conditions, now shows a gyre near the end of the dock. On the other hand, a considerable increase (about 30%) in the velocities near the end of the breakwater and in the main channel of the estuary has been observed after the building of the dock. A stronger bottom shear stress has been generated in the estuary areas where the velocity increased. The bottom shear stress increase was particularly great (over 100%) near the end of the dock. This increase in the shear stress produced bottom erosion and matter resuspension, and consequently major changes in the bathymetry. In addition, in situ sedimentary measurements carried out by Lopez-Jamar (1996) corroborate the bottom erosion in the main chanel of the estuary and at the end of the dock produced by the velocity increase generated by the building of the breakwater.SapientiaGómez-Gesteira, MonchoDecastro, MaitePrego, RicardoMartins, Flávio Augusto Bastos da Cruz2009-02-13T17:10:01Z20082008-01-01T00:00:00Zinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10400.1/168engSCIENTIA MARINAScientia Marina. - Barcelona. - Vol. 66, nº. 4 (2002), p. 337-346info: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:RCAAP2023-07-24T10:10:53Zoai:sapientia.ualg.pt:10400.1/168Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireopendoar:71602024-03-19T19:54:34.724485Repositório 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 Influence of the Barrie de la Maza dock on the circulation pattern of the Ría of a Coruña (NW-Spain)
title Influence of the Barrie de la Maza dock on the circulation pattern of the Ría of a Coruña (NW-Spain)
spellingShingle Influence of the Barrie de la Maza dock on the circulation pattern of the Ría of a Coruña (NW-Spain)
Gómez-Gesteira, Moncho
Estuários
Quebra mares
532
title_short Influence of the Barrie de la Maza dock on the circulation pattern of the Ría of a Coruña (NW-Spain)
title_full Influence of the Barrie de la Maza dock on the circulation pattern of the Ría of a Coruña (NW-Spain)
title_fullStr Influence of the Barrie de la Maza dock on the circulation pattern of the Ría of a Coruña (NW-Spain)
title_full_unstemmed Influence of the Barrie de la Maza dock on the circulation pattern of the Ría of a Coruña (NW-Spain)
title_sort Influence of the Barrie de la Maza dock on the circulation pattern of the Ría of a Coruña (NW-Spain)
author Gómez-Gesteira, Moncho
author_facet Gómez-Gesteira, Moncho
Decastro, Maite
Prego, Ricardo
Martins, Flávio Augusto Bastos da Cruz
author_role author
author2 Decastro, Maite
Prego, Ricardo
Martins, Flávio Augusto Bastos da Cruz
author2_role author
author
author
dc.contributor.none.fl_str_mv Sapientia
dc.contributor.author.fl_str_mv Gómez-Gesteira, Moncho
Decastro, Maite
Prego, Ricardo
Martins, Flávio Augusto Bastos da Cruz
dc.subject.por.fl_str_mv Estuários
Quebra mares
532
topic Estuários
Quebra mares
532
description A 3D hydrodynamical model is applied to the ria of A Coruña to analyze the evolution of the circulation pattern in the ria after the building of a breakwater (Barrie de la Maza dock) in the sixties. This circulation pattern has changed greatly. On the one hand, the circulation, which was almost parallel to the shore line under the original conditions, now shows a gyre near the end of the dock. On the other hand, a considerable increase (about 30%) in the velocities near the end of the breakwater and in the main channel of the estuary has been observed after the building of the dock. A stronger bottom shear stress has been generated in the estuary areas where the velocity increased. The bottom shear stress increase was particularly great (over 100%) near the end of the dock. This increase in the shear stress produced bottom erosion and matter resuspension, and consequently major changes in the bathymetry. In addition, in situ sedimentary measurements carried out by Lopez-Jamar (1996) corroborate the bottom erosion in the main chanel of the estuary and at the end of the dock produced by the velocity increase generated by the building of the breakwater.
publishDate 2008
dc.date.none.fl_str_mv 2008
2008-01-01T00:00:00Z
2009-02-13T17:10:01Z
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
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status_str publishedVersion
dc.identifier.uri.fl_str_mv http://hdl.handle.net/10400.1/168
url http://hdl.handle.net/10400.1/168
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv SCIENTIA MARINAScientia Marina. - Barcelona. - Vol. 66, nº. 4 (2002), p. 337-346
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eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
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