The morphodynamic responses of artificial embayed beaches to storm events

The morphological changes caused by storm events in two Barcelona beaches were recorded using video monitoring techniques during the period 2001–2006. Changes in shoreline position and configuration and submerged bar position and shape were analyzed during the 25 major storm events that occurred dur...

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Main Authors: E. Ojeda, J. Guillén, F. Ribas
Format: Article
Language:English
Published: Copernicus Publications 2010-09-01
Series:Advances in Geosciences
Online Access:http://www.adv-geosci.net/26/99/2010/adgeo-26-99-2010.pdf
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spelling doaj-0390a11a68c24b3eb3d490843920a5a92020-11-24T23:40:18ZengCopernicus PublicationsAdvances in Geosciences1680-73401680-73592010-09-01269910310.5194/adgeo-26-99-2010The morphodynamic responses of artificial embayed beaches to storm eventsE. Ojeda0J. Guillén1F. Ribas2Institut de Ciències del Mar (CSIC), Passeig Marítim de la Barceloneta 37–49, 08003 Barcelona, SpainInstitut de Ciències del Mar (CSIC), Passeig Marítim de la Barceloneta 37–49, 08003 Barcelona, SpainInstitut de Ciències del Mar (CSIC), Passeig Marítim de la Barceloneta 37–49, 08003 Barcelona, SpainThe morphological changes caused by storm events in two Barcelona beaches were recorded using video monitoring techniques during the period 2001–2006. Changes in shoreline position and configuration and submerged bar position and shape were analyzed during the 25 major storm events that occurred during the study period. Beach responses to storms were grouped into three categories: shoreline advance or retreat (including rotation), sandbar migration and/or configuration change (linear or crescentic shape) and formation of megacusps. This work provides examples of the differential adaptation of both beaches to the same storm and of some unexpected morphological responses of both beaches. The response of the beach to storm events is not straightforward because wave conditions are not the only relevant parameter to be considered. In particular, in such embayed beaches it is crucial to take into account their specific morphodynamic configuration prior to the storm.http://www.adv-geosci.net/26/99/2010/adgeo-26-99-2010.pdf
collection DOAJ
language English
format Article
sources DOAJ
author E. Ojeda
J. Guillén
F. Ribas
spellingShingle E. Ojeda
J. Guillén
F. Ribas
The morphodynamic responses of artificial embayed beaches to storm events
Advances in Geosciences
author_facet E. Ojeda
J. Guillén
F. Ribas
author_sort E. Ojeda
title The morphodynamic responses of artificial embayed beaches to storm events
title_short The morphodynamic responses of artificial embayed beaches to storm events
title_full The morphodynamic responses of artificial embayed beaches to storm events
title_fullStr The morphodynamic responses of artificial embayed beaches to storm events
title_full_unstemmed The morphodynamic responses of artificial embayed beaches to storm events
title_sort morphodynamic responses of artificial embayed beaches to storm events
publisher Copernicus Publications
series Advances in Geosciences
issn 1680-7340
1680-7359
publishDate 2010-09-01
description The morphological changes caused by storm events in two Barcelona beaches were recorded using video monitoring techniques during the period 2001–2006. Changes in shoreline position and configuration and submerged bar position and shape were analyzed during the 25 major storm events that occurred during the study period. Beach responses to storms were grouped into three categories: shoreline advance or retreat (including rotation), sandbar migration and/or configuration change (linear or crescentic shape) and formation of megacusps. This work provides examples of the differential adaptation of both beaches to the same storm and of some unexpected morphological responses of both beaches. The response of the beach to storm events is not straightforward because wave conditions are not the only relevant parameter to be considered. In particular, in such embayed beaches it is crucial to take into account their specific morphodynamic configuration prior to the storm.
url http://www.adv-geosci.net/26/99/2010/adgeo-26-99-2010.pdf
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