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Advisor(s)
Abstract(s)
Overwash prediction is very important for coastal zone
management. This work intends to identify alongshore variations in
storm impact and evaluate the role of sub-aerial and submerged
morphologies in overwash occurrence. For this study, 24 cross-shore
topo-bathymetric profiles were set on Barreta Island (Ria Formosa
barrier island system, Portugal). Pre- and post-overwash surveys were
made between August 2012 and April 2013. During overwash events,
tidal levels and wave parameters at breaking were obtained. Overwash
occurred under storm and non-storm conditions, the latter coincident
with spring high-tide. Beach morphology was spatially variable, and
changeable from one overwash episode to the next. Predictions of
overwash occurrence were made using the Overwash Potential, defined
as the difference between runup and barrier elevation. Several runup
equations were tested, and the results compared to the actual
observations. The selected predictor provided an accuracy of 88% for
the identification of the locations where overwash occurred. This study
proves that nearshore and foreshore morphologies have a major impact
on the longshore distribution of overwash.
Description
Keywords
SWAN Runup Storm Coastal hazards
Citation
Publisher
Laboratório Nacional de Energia e Geologia