Combined beach - inner shelf erosion in short and medium term (Maspalomas, Canary Islands)

The analysis of the accurate topo-bathymetric digital elevation model (DEM), the cartography of the submarine sedimentary cover and the monitoring of short (seasonal) and medium-term (2000-2009) morphological changes have permitted depicting the erosional trend in the short and medium-term of the Ma...

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Autores:
Fontán, A
Alcántara-Carrió, J
Correa-Arango, Ivan D.
Tipo de recurso:
Fecha de publicación:
2012
Institución:
Universidad EAFIT
Repositorio:
Repositorio EAFIT
Idioma:
eng
OAI Identifier:
oai:repository.eafit.edu.co:10784/1598
Acceso en línea:
http://hdl.handle.net/10784/1598
Palabra clave:
GEOMORFOLOGÍA
EROSIÓN COSTERA
MODELOS MATEMÁTICOS
PLATAFORMA CONTINENTAL
REGIONES COSTERAS
VIENTOS - MEDICIONES
Coastal geomorphology
Sediments
Budget
Storms
Climatic change
Geomorphology
Coast changes
Mathematical models
Continental shelf
Coastal regions
Winds - Measurement
Rights
License
Acceso abierto
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spelling 2014-05-09T22:05:19Z2012-12-012014-05-09T22:05:19Z1695-6133http://hdl.handle.net/10784/159810.1344/105.000001756The analysis of the accurate topo-bathymetric digital elevation model (DEM), the cartography of the submarine sedimentary cover and the monitoring of short (seasonal) and medium-term (2000-2009) morphological changes have permitted depicting the erosional trend in the short and medium-term of the Maspalomas sedimentary system. Short-term analysis showed intense sedimentary fluxes between the beaches and the inner shelf, and sedimentary exchanges with other sectors of the inner shelf, while the steep slope inner shelf fronting La Bajeta cape was identified as a sink area. In the medium-term the sediment budget showed high erosion of the supratidal and intertidal sectors of the beaches due to storm waves in the 2005-2006 winter, followed by accretion over the next four years, but which did not reach the initial sedimentary state. The inner shelf and subtidal sector of the beaches showed negative budgets in the short and medium-term. Interannual variability of the wave and wind regimes determines decadal beach erosion-accretion cycles, while long-term climatic change, evidenced at the study area by a decrease of trade winds and NE wave intensity in 2005, is expected to produce a possible increase of erosion at the El Inglés inner shelf and consequently a decrease in sediment inputs to the El Inglés beach and Maspalomas dune field. Finally, the influence of the geological heritage is depicted by the Fataga gully’s control of the present coastal morphology, and by the island relief control of the wind, waves and current directions in the study area.engFaculty of Geology, Martí i FranquèsGeologica acta: an international earth science journal, ISSN 1695-6133, Vol. 10, Nº. 4, 2012 , págs. 411-42310.1344/105.000001756Combined beach - inner shelf erosion in short and medium term (Maspalomas, Canary Islands)info:eu-repo/semantics/articlearticleinfo:eu-repo/semantics/publishedVersionpublishedVersionArtículohttp://purl.org/coar/version/c_970fb48d4fbd8a85http://purl.org/coar/resource_type/c_6501http://purl.org/coar/resource_type/c_2df8fbb1Acceso abiertohttp://purl.org/coar/access_right/c_abf2GEOMORFOLOGÍAEROSIÓN COSTERAMODELOS MATEMÁTICOSPLATAFORMA CONTINENTALREGIONES COSTERASVIENTOS - MEDICIONESCoastal geomorphologySedimentsBudgetStormsClimatic changeGeomorphologyCoast changesMathematical modelsContinental shelfCoastal regionsWinds - MeasurementUniversidad EAFIT. Departamento de GeologíaIvan D. Correa-Arango (icorrea@eafit.edu.co)Fontán, Aef7bd20d-473c-4ffd-b89a-ce6bccb64253-1Alcántara-Carrió, Je5e13b6a-fa8c-465e-a7b9-d6939d43e9c3-1Correa-Arango, Ivan D.20e7a8ee-1ba9-480b-9fcb-10612a0b5213-1Ciencias del MarGeologica acta: an international earth science journalLICENSElicense.txtlicense.txttext/plain; charset=utf-81748https://repository.eafit.edu.co/bitstreams/053bda95-0931-47b1-9aba-be230cedcb4a/download8a4605be74aa9ea9d79846c1fba20a33MD52ORIGINALCombined beach - inner shelf erosion in short and medium term.pdfCombined beach - inner shelf erosion in short and medium term.pdfTexto completoapplication/pdf3284604https://repository.eafit.edu.co/bitstreams/a47b283a-e1d5-4cfe-b47e-2fedc0488e4c/download56201aec56e0fcc232faa766ee58e16aMD5310784/1598oai:repository.eafit.edu.co:10784/15982024-12-04 11:49:08.825open.accesshttps://repository.eafit.edu.coRepositorio Institucional Universidad EAFITrepositorio@eafit.edu.co
dc.title.eng.fl_str_mv Combined beach - inner shelf erosion in short and medium term (Maspalomas, Canary Islands)
title Combined beach - inner shelf erosion in short and medium term (Maspalomas, Canary Islands)
spellingShingle Combined beach - inner shelf erosion in short and medium term (Maspalomas, Canary Islands)
GEOMORFOLOGÍA
EROSIÓN COSTERA
MODELOS MATEMÁTICOS
PLATAFORMA CONTINENTAL
REGIONES COSTERAS
VIENTOS - MEDICIONES
Coastal geomorphology
Sediments
Budget
Storms
Climatic change
Geomorphology
Coast changes
Mathematical models
Continental shelf
Coastal regions
Winds - Measurement
title_short Combined beach - inner shelf erosion in short and medium term (Maspalomas, Canary Islands)
title_full Combined beach - inner shelf erosion in short and medium term (Maspalomas, Canary Islands)
title_fullStr Combined beach - inner shelf erosion in short and medium term (Maspalomas, Canary Islands)
title_full_unstemmed Combined beach - inner shelf erosion in short and medium term (Maspalomas, Canary Islands)
title_sort Combined beach - inner shelf erosion in short and medium term (Maspalomas, Canary Islands)
dc.creator.fl_str_mv Fontán, A
Alcántara-Carrió, J
Correa-Arango, Ivan D.
dc.contributor.department.spa.fl_str_mv Universidad EAFIT. Departamento de Geología
dc.contributor.eafitauthor.spa.fl_str_mv Ivan D. Correa-Arango (icorrea@eafit.edu.co)
dc.contributor.author.spa.fl_str_mv Fontán, A
Alcántara-Carrió, J
Correa-Arango, Ivan D.
dc.contributor.researchgroup.spa.fl_str_mv Ciencias del Mar
dc.subject.lemb.spa.fl_str_mv GEOMORFOLOGÍA
EROSIÓN COSTERA
MODELOS MATEMÁTICOS
PLATAFORMA CONTINENTAL
REGIONES COSTERAS
VIENTOS - MEDICIONES
topic GEOMORFOLOGÍA
EROSIÓN COSTERA
MODELOS MATEMÁTICOS
PLATAFORMA CONTINENTAL
REGIONES COSTERAS
VIENTOS - MEDICIONES
Coastal geomorphology
Sediments
Budget
Storms
Climatic change
Geomorphology
Coast changes
Mathematical models
Continental shelf
Coastal regions
Winds - Measurement
dc.subject.keyword.eng.fl_str_mv Coastal geomorphology
Sediments
Budget
Storms
Climatic change
Geomorphology
Coast changes
Mathematical models
Continental shelf
Coastal regions
Winds - Measurement
description The analysis of the accurate topo-bathymetric digital elevation model (DEM), the cartography of the submarine sedimentary cover and the monitoring of short (seasonal) and medium-term (2000-2009) morphological changes have permitted depicting the erosional trend in the short and medium-term of the Maspalomas sedimentary system. Short-term analysis showed intense sedimentary fluxes between the beaches and the inner shelf, and sedimentary exchanges with other sectors of the inner shelf, while the steep slope inner shelf fronting La Bajeta cape was identified as a sink area. In the medium-term the sediment budget showed high erosion of the supratidal and intertidal sectors of the beaches due to storm waves in the 2005-2006 winter, followed by accretion over the next four years, but which did not reach the initial sedimentary state. The inner shelf and subtidal sector of the beaches showed negative budgets in the short and medium-term. Interannual variability of the wave and wind regimes determines decadal beach erosion-accretion cycles, while long-term climatic change, evidenced at the study area by a decrease of trade winds and NE wave intensity in 2005, is expected to produce a possible increase of erosion at the El Inglés inner shelf and consequently a decrease in sediment inputs to the El Inglés beach and Maspalomas dune field. Finally, the influence of the geological heritage is depicted by the Fataga gully’s control of the present coastal morphology, and by the island relief control of the wind, waves and current directions in the study area.
publishDate 2012
dc.date.issued.none.fl_str_mv 2012-12-01
dc.date.available.none.fl_str_mv 2014-05-09T22:05:19Z
dc.date.accessioned.none.fl_str_mv 2014-05-09T22:05:19Z
dc.type.eng.fl_str_mv info:eu-repo/semantics/article
article
info:eu-repo/semantics/publishedVersion
publishedVersion
dc.type.coarversion.fl_str_mv http://purl.org/coar/version/c_970fb48d4fbd8a85
dc.type.coar.fl_str_mv http://purl.org/coar/resource_type/c_6501
http://purl.org/coar/resource_type/c_2df8fbb1
dc.type.local.spa.fl_str_mv Artículo
status_str publishedVersion
dc.identifier.issn.none.fl_str_mv 1695-6133
dc.identifier.uri.none.fl_str_mv http://hdl.handle.net/10784/1598
dc.identifier.doi.none.fl_str_mv 10.1344/105.000001756
identifier_str_mv 1695-6133
10.1344/105.000001756
url http://hdl.handle.net/10784/1598
dc.language.iso.eng.fl_str_mv eng
language eng
dc.relation.ispartof.eng.fl_str_mv Geologica acta: an international earth science journal, ISSN 1695-6133, Vol. 10, Nº. 4, 2012 , págs. 411-423
dc.relation.uri.none.fl_str_mv 10.1344/105.000001756
dc.rights.coar.fl_str_mv http://purl.org/coar/access_right/c_abf2
dc.rights.local.spa.fl_str_mv Acceso abierto
rights_invalid_str_mv Acceso abierto
http://purl.org/coar/access_right/c_abf2
dc.publisher.none.fl_str_mv Faculty of Geology, Martí i Franquès
publisher.none.fl_str_mv Faculty of Geology, Martí i Franquès
institution Universidad EAFIT
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