Are wind wave heights increasing in south-eastern south American continental shelf between 32°S and 40°S?

In this paper, a possible increase in wind wave heights in the south-eastern south American continental shelf between 32°S and 40°S is investigated. Both time series of in situ (1996-2006) and topex (1993-2001) annual mean significant wave heights gathered at the continental shelf and adjacent ocean...

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Autores principales: Dragani, Walter César, Martin, Paula Beatriz, Simionato, Claudia Gloria
Publicado: 2010
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Acceso en línea:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_02784343_v30_n5_p481_Dragani
http://hdl.handle.net/20.500.12110/paper_02784343_v30_n5_p481_Dragani
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spelling paper:paper_02784343_v30_n5_p481_Dragani2023-06-08T15:26:49Z Are wind wave heights increasing in south-eastern south American continental shelf between 32°S and 40°S? Dragani, Walter César Martin, Paula Beatriz Simionato, Claudia Gloria South-western Atlantic Ocean SWAN model Wind wave height trend annual variation atmospheric circulation coastal erosion continental shelf El Nino-Southern Oscillation littoral environment nearshore environment satellite data Southern Hemisphere surface wind time series wave height wave modeling wind wave Rio de la Plata In this paper, a possible increase in wind wave heights in the south-eastern south American continental shelf between 32°S and 40°S is investigated. Both time series of in situ (1996-2006) and topex (1993-2001) annual mean significant wave heights gathered at the continental shelf and adjacent ocean present apparent positive trends. Even though these trends are not statistically different from zero, it must be taken into account that the available in situ and satellite data have a short span and, moreover, in situ data present several gaps. Several papers presented evidence about a possible change on the low atmospheric circulation in this region of the southern hemisphere. Consequently, a weak increase in wave height might be occurring, which would be hard to quantify due to the shortness and the insufficiency of the available observations. In order to study a possible trend in mean annual wind wave heights simulating waves nearshore (swan) model forced with ncep/ncar surface wind was implemented in a regional domain for the period 1971-2005. The annual root-mean-square heights of the simulated wave show significant trends at several locations of the inner continental shelf and the adjacent ocean. The most significant increase is observed between 1991-2000 and 1981-1990 decades. The largest difference (0.20 m, 9%) occurs around 34°S-48°W. The wave height increase is somewhat lower, 7%, in the continental shelf and in the río de la plata estuary. The annual mean energy density (spatially averaged) also presents a significant positive trend (0.036 m2/yr) and relatively high inter-annual variability. The possible link between this inter-annual variability and el niño-southern oscillation (enso) was investigated but no apparent relationship was found. A possible increase in the annual mean energy density of waves would be able to produce changes in the littoral processes and, consequently, in the erosion of the coast. © 2010 Elsevier Ltd. All rights reserved. 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. 2010 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_02784343_v30_n5_p481_Dragani http://hdl.handle.net/20.500.12110/paper_02784343_v30_n5_p481_Dragani
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic South-western Atlantic Ocean
SWAN model
Wind wave height trend
annual variation
atmospheric circulation
coastal erosion
continental shelf
El Nino-Southern Oscillation
littoral environment
nearshore environment
satellite data
Southern Hemisphere
surface wind
time series
wave height
wave modeling
wind wave
Rio de la Plata
spellingShingle South-western Atlantic Ocean
SWAN model
Wind wave height trend
annual variation
atmospheric circulation
coastal erosion
continental shelf
El Nino-Southern Oscillation
littoral environment
nearshore environment
satellite data
Southern Hemisphere
surface wind
time series
wave height
wave modeling
wind wave
Rio de la Plata
Dragani, Walter César
Martin, Paula Beatriz
Simionato, Claudia Gloria
Are wind wave heights increasing in south-eastern south American continental shelf between 32°S and 40°S?
topic_facet South-western Atlantic Ocean
SWAN model
Wind wave height trend
annual variation
atmospheric circulation
coastal erosion
continental shelf
El Nino-Southern Oscillation
littoral environment
nearshore environment
satellite data
Southern Hemisphere
surface wind
time series
wave height
wave modeling
wind wave
Rio de la Plata
description In this paper, a possible increase in wind wave heights in the south-eastern south American continental shelf between 32°S and 40°S is investigated. Both time series of in situ (1996-2006) and topex (1993-2001) annual mean significant wave heights gathered at the continental shelf and adjacent ocean present apparent positive trends. Even though these trends are not statistically different from zero, it must be taken into account that the available in situ and satellite data have a short span and, moreover, in situ data present several gaps. Several papers presented evidence about a possible change on the low atmospheric circulation in this region of the southern hemisphere. Consequently, a weak increase in wave height might be occurring, which would be hard to quantify due to the shortness and the insufficiency of the available observations. In order to study a possible trend in mean annual wind wave heights simulating waves nearshore (swan) model forced with ncep/ncar surface wind was implemented in a regional domain for the period 1971-2005. The annual root-mean-square heights of the simulated wave show significant trends at several locations of the inner continental shelf and the adjacent ocean. The most significant increase is observed between 1991-2000 and 1981-1990 decades. The largest difference (0.20 m, 9%) occurs around 34°S-48°W. The wave height increase is somewhat lower, 7%, in the continental shelf and in the río de la plata estuary. The annual mean energy density (spatially averaged) also presents a significant positive trend (0.036 m2/yr) and relatively high inter-annual variability. The possible link between this inter-annual variability and el niño-southern oscillation (enso) was investigated but no apparent relationship was found. A possible increase in the annual mean energy density of waves would be able to produce changes in the littoral processes and, consequently, in the erosion of the coast. © 2010 Elsevier Ltd. All rights reserved.
author Dragani, Walter César
Martin, Paula Beatriz
Simionato, Claudia Gloria
author_facet Dragani, Walter César
Martin, Paula Beatriz
Simionato, Claudia Gloria
author_sort Dragani, Walter César
title Are wind wave heights increasing in south-eastern south American continental shelf between 32°S and 40°S?
title_short Are wind wave heights increasing in south-eastern south American continental shelf between 32°S and 40°S?
title_full Are wind wave heights increasing in south-eastern south American continental shelf between 32°S and 40°S?
title_fullStr Are wind wave heights increasing in south-eastern south American continental shelf between 32°S and 40°S?
title_full_unstemmed Are wind wave heights increasing in south-eastern south American continental shelf between 32°S and 40°S?
title_sort are wind wave heights increasing in south-eastern south american continental shelf between 32°s and 40°s?
publishDate 2010
url https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_02784343_v30_n5_p481_Dragani
http://hdl.handle.net/20.500.12110/paper_02784343_v30_n5_p481_Dragani
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AT martinpaulabeatriz arewindwaveheightsincreasinginsoutheasternsouthamericancontinentalshelfbetween32sand40s
AT simionatoclaudiagloria arewindwaveheightsincreasinginsoutheasternsouthamericancontinentalshelfbetween32sand40s
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