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...
- 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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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 |
bitstream.url.fl_str_mv |
https://repository.eafit.edu.co/bitstreams/053bda95-0931-47b1-9aba-be230cedcb4a/download https://repository.eafit.edu.co/bitstreams/a47b283a-e1d5-4cfe-b47e-2fedc0488e4c/download |
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MD5 MD5 |
repository.name.fl_str_mv |
Repositorio Institucional Universidad EAFIT |
repository.mail.fl_str_mv |
repositorio@eafit.edu.co |
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1818102415556083712 |