Wind-wave climate change and increasing erosion in the outer Río de la Plata, Argentina

The coastal area of Samborombón Bay ends in a short cliff which, during the last decades, has been undergoing an increased retrogression of approximately 8.2m decade -1. The aim of this paper is to investigate whether this accelerated erosion can be related to an apparent wind-wave climate change, w...

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Autores principales: Codignotto, J.O., Dragani, W.C., Martin, P.B., Simionato, C.G., Medina, R.A., Alonso, G.
Formato: JOUR
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_02784343_v38_n_p110_Codignotto
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spelling todo:paper_02784343_v38_n_p110_Codignotto2023-10-03T15:17:01Z Wind-wave climate change and increasing erosion in the outer Río de la Plata, Argentina Codignotto, J.O. Dragani, W.C. Martin, P.B. Simionato, C.G. Medina, R.A. Alonso, G. Erosion Río de la Plata Samborombón Bay SWAN wave model Wind-wave climate change bay cliff climate change erosion rate retrogression storm surge wave climate wave modeling wave propagation Argentina Buenos Aires [Argentina] Rio de la Plata Samborombon Bay The coastal area of Samborombón Bay ends in a short cliff which, during the last decades, has been undergoing an increased retrogression of approximately 8.2m decade -1. The aim of this paper is to investigate whether this accelerated erosion can be related to an apparent wind-wave climate change, which has been recently reported for the Río de la Plata region. A numerical study with SWAN wave model for the period 1971-2005 drives to positive trends in the frequency of occurrence and heights of waves propagating from the E and ESE. Particularly, the number of cases of high waves from those directions displays a significant increment. In addition, previous papers have reported an increment of the frequency, height and duration of the storm surges in the Río de la Plata, so as a rise of the mean sea level in the region. It is concluded that the combination of those three factors acting together constitutes a powerful and effective mechanism which is likely responsible for the observed increasing erosion in Samborombón Bay. © 2012 Elsevier Ltd. Fil:Codignotto, J.O. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Dragani, W.C. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Martin, P.B. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Simionato, C.G. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_02784343_v38_n_p110_Codignotto
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Erosion
Río de la Plata
Samborombón Bay
SWAN wave model
Wind-wave climate change
bay
cliff
climate change
erosion rate
retrogression
storm surge
wave climate
wave modeling
wave propagation
Argentina
Buenos Aires [Argentina]
Rio de la Plata
Samborombon Bay
spellingShingle Erosion
Río de la Plata
Samborombón Bay
SWAN wave model
Wind-wave climate change
bay
cliff
climate change
erosion rate
retrogression
storm surge
wave climate
wave modeling
wave propagation
Argentina
Buenos Aires [Argentina]
Rio de la Plata
Samborombon Bay
Codignotto, J.O.
Dragani, W.C.
Martin, P.B.
Simionato, C.G.
Medina, R.A.
Alonso, G.
Wind-wave climate change and increasing erosion in the outer Río de la Plata, Argentina
topic_facet Erosion
Río de la Plata
Samborombón Bay
SWAN wave model
Wind-wave climate change
bay
cliff
climate change
erosion rate
retrogression
storm surge
wave climate
wave modeling
wave propagation
Argentina
Buenos Aires [Argentina]
Rio de la Plata
Samborombon Bay
description The coastal area of Samborombón Bay ends in a short cliff which, during the last decades, has been undergoing an increased retrogression of approximately 8.2m decade -1. The aim of this paper is to investigate whether this accelerated erosion can be related to an apparent wind-wave climate change, which has been recently reported for the Río de la Plata region. A numerical study with SWAN wave model for the period 1971-2005 drives to positive trends in the frequency of occurrence and heights of waves propagating from the E and ESE. Particularly, the number of cases of high waves from those directions displays a significant increment. In addition, previous papers have reported an increment of the frequency, height and duration of the storm surges in the Río de la Plata, so as a rise of the mean sea level in the region. It is concluded that the combination of those three factors acting together constitutes a powerful and effective mechanism which is likely responsible for the observed increasing erosion in Samborombón Bay. © 2012 Elsevier Ltd.
format JOUR
author Codignotto, J.O.
Dragani, W.C.
Martin, P.B.
Simionato, C.G.
Medina, R.A.
Alonso, G.
author_facet Codignotto, J.O.
Dragani, W.C.
Martin, P.B.
Simionato, C.G.
Medina, R.A.
Alonso, G.
author_sort Codignotto, J.O.
title Wind-wave climate change and increasing erosion in the outer Río de la Plata, Argentina
title_short Wind-wave climate change and increasing erosion in the outer Río de la Plata, Argentina
title_full Wind-wave climate change and increasing erosion in the outer Río de la Plata, Argentina
title_fullStr Wind-wave climate change and increasing erosion in the outer Río de la Plata, Argentina
title_full_unstemmed Wind-wave climate change and increasing erosion in the outer Río de la Plata, Argentina
title_sort wind-wave climate change and increasing erosion in the outer río de la plata, argentina
url http://hdl.handle.net/20.500.12110/paper_02784343_v38_n_p110_Codignotto
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