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Advisor(s)
Abstract(s)
This study reports the medium-term evolution of a sandy backbarrier and its relation with prevailing wind
conditions. Obtained results demonstrated that Ancão backbarrier does not behave as a scale-down version of
higher energy fetch-limited or oceanic beaches, being considered as a low-energy beach with extremely low
wind-induced wave conditions. Volumetric changes during the three years monitoring were small, and the
analysis of low-scale changes was divided into four beach compartment: upper beach, beach face, tidal flat, sand
bank. There was no significant correlation between prevailing wind conditions, volume and grain-size variation,
neither a marked seasonal pattern. Some wind-induced beach changes were perceptive in the grain size
variations, related mostly to aeolian offshore sediment transport. Morphological changes were similar in the
upper part of the profile, including upper beach and beach face, with changes mostly related to wind and windwaves
energy. The lower part of the profile, which includes the tidal flat and the sand bank, frequently react
independently from the upper part of the profile, although, sediment exchange between them was noticed during
extreme conditions. The lower part of the profile had larger volumetric variability, without any evident wind
dominance.
The studied beach revealed high morphologic resilience, yet the overall quantities of sediment transported
between 2005 and 2008 has particular relevance in the local coastal management context. Further research is
needed to develop a broad-scale model of fetch-limited beaches, including the less energetic settings of the
spectra such as backbarrier environments.
Description
Keywords
Fetch-limited Small-scale Wind
Citation
Publisher
Coastal Education and Research Foundation