Overwash hazard assessment

Overwash is a natural storm-related process that occurs when wave runup overcomes the dune crest. Because coastlines are globally occupied, overwash is a hazardous process and there is a need to identify vulnerable areas. This study proposes a method to detect overwash-prone areas in the Ancão peni...

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Main Authors: B.A. RODRIGUES, A. MATIAS, Ó. FERREIRA
Format: Article
Language:English
Published: Universitat de Barcelona (UB), Geociències Barcelona (Geo3BCN), Institut de Diagnosi Ambiental i Estudis de l'Aigua (IDAEA), Universitat Autònoma de Barcelona (UAB) 2013-07-01
Series:Geologica Acta
Subjects:
Online Access:https://revistes.ub.edu/index.php/GEOACTA/article/view/7450
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author B.A. RODRIGUES
A. MATIAS
Ó. FERREIRA
author_facet B.A. RODRIGUES
A. MATIAS
Ó. FERREIRA
author_sort B.A. RODRIGUES
collection DOAJ
description Overwash is a natural storm-related process that occurs when wave runup overcomes the dune crest. Because coastlines are globally occupied, overwash is a hazardous process and there is a need to identify vulnerable areas. This study proposes a method to detect overwash-prone areas in the Ancão peninsula, Portugal, and eventually outlines a vulnerability map. Dune base (DLOW) and crest (DHIGH) topography were surveyed. Three different storm scenarios (5-, 10- and 25- year return period storms) and associated waves and sea level were determined. According to these data, extreme wave runup (RHIGH) was calculated by a parameterisation set for intermediate-reflective beaches. The maps for collision and overwash regimes were designed by comparing RHIGH values with DLOW and DHIGH. Almost the entire dune base along the peninsula is vulnerable to collision regime. The overwash process was identified mainly along the tidal inlet hazard area and within the human-occupied portion of the beach, where overwash is expected to occur within 5 years of return period. The developed method considers the main overwash driving forces and proved to identify hazardous areas previously observed in the area. Occasional differences between modelled and observed overwash areas can be attributable to equipment errors, morphology interpretation subjectivity and maladjustments in runup parameterisation. Nevertheless, the method proved to be effective in reproducing the overall Ancão peninsula vulnerability and can be widely applied. Therefore, it is a simple and potentially important tool for coastal management that enables mitigation strategies for occupied coasts and assessment of geological and ecological consequences in natural areas.
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spelling doaj.art-f47a7551929e471fb9242e99a4f0760d2023-10-20T07:05:40ZengUniversitat de Barcelona (UB), Geociències Barcelona (Geo3BCN), Institut de Diagnosi Ambiental i Estudis de l'Aigua (IDAEA), Universitat Autònoma de Barcelona (UAB)Geologica Acta1696-57282013-07-01104Overwash hazard assessmentB.A. RODRIGUES0A. MATIAS1Ó. FERREIRA2FCMA/CIMA, Universidade do Algarve, Campus de Gambelas 8005-139, Faro, Portugal. Fax: +351 289 800696.FCMA/CIMA, Universidade do Algarve, Campus de Gambelas 8005-139, Faro, Portugal. Fax: +351 289 800696.FCMA/CIMA, Universidade do Algarve, Campus de Gambelas 8005-139, Faro, Portugal. Fax: +351 289 800696. Overwash is a natural storm-related process that occurs when wave runup overcomes the dune crest. Because coastlines are globally occupied, overwash is a hazardous process and there is a need to identify vulnerable areas. This study proposes a method to detect overwash-prone areas in the Ancão peninsula, Portugal, and eventually outlines a vulnerability map. Dune base (DLOW) and crest (DHIGH) topography were surveyed. Three different storm scenarios (5-, 10- and 25- year return period storms) and associated waves and sea level were determined. According to these data, extreme wave runup (RHIGH) was calculated by a parameterisation set for intermediate-reflective beaches. The maps for collision and overwash regimes were designed by comparing RHIGH values with DLOW and DHIGH. Almost the entire dune base along the peninsula is vulnerable to collision regime. The overwash process was identified mainly along the tidal inlet hazard area and within the human-occupied portion of the beach, where overwash is expected to occur within 5 years of return period. The developed method considers the main overwash driving forces and proved to identify hazardous areas previously observed in the area. Occasional differences between modelled and observed overwash areas can be attributable to equipment errors, morphology interpretation subjectivity and maladjustments in runup parameterisation. Nevertheless, the method proved to be effective in reproducing the overall Ancão peninsula vulnerability and can be widely applied. Therefore, it is a simple and potentially important tool for coastal management that enables mitigation strategies for occupied coasts and assessment of geological and ecological consequences in natural areas. https://revistes.ub.edu/index.php/GEOACTA/article/view/7450OverwashStorm SurgeRunupBarrier IslandGIS
spellingShingle B.A. RODRIGUES
A. MATIAS
Ó. FERREIRA
Overwash hazard assessment
Geologica Acta
Overwash
Storm Surge
Runup
Barrier Island
GIS
title Overwash hazard assessment
title_full Overwash hazard assessment
title_fullStr Overwash hazard assessment
title_full_unstemmed Overwash hazard assessment
title_short Overwash hazard assessment
title_sort overwash hazard assessment
topic Overwash
Storm Surge
Runup
Barrier Island
GIS
url https://revistes.ub.edu/index.php/GEOACTA/article/view/7450
work_keys_str_mv AT barodrigues overwashhazardassessment
AT amatias overwashhazardassessment
AT oferreira overwashhazardassessment