Extreme storm surges in the south of Brazil: atmospheric conditions and shore erosion
Autor(a) principal: | |
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Data de Publicação: | 2009 |
Outros Autores: | , |
Tipo de documento: | Artigo |
Idioma: | eng |
Título da fonte: | Repositório Institucional da FURG (RI FURG) |
Texto Completo: | http://repositorio.furg.br/handle/1/2865 |
Resumo: | The region under study is regularly subject to the occurrence of storms associated with frontal systems and extratropical cyclones, since it is located near one of the cyclogenetic regions in South America. These storms can generate storm surges that cause anomalous high sea level rises on Cassino Beach. The use of reanalysis data along with an efficient technique for the location of the cyclone, using a vorticity threshold, has provided a new classification based upon the trajectories of events that produce positive sea level variation. Three patterns have been identified: 1) Cyclogenesis to the south of Argentina with displacement to the east and a trajectory between 47.5ºS and 57.5ºS; 2) Cyclogenesis to the south of Uruguay with displacement to the east and a trajectory between 35ºS and 42.5ºS; and 3) Cyclogenesis to the south of Uruguay with displacement to the southeast and a trajectory between 35ºS and 57.5ºS. Maximum water level elevation above the mean sea level and beach erosion were associated, respectively, with winter and summer storms. Cassino beach displayed a seasonal morphological behavior, with short periods of episodic erosion associated with winter storm events followed by long periods of accretion characterized by the dominance of fair weather conditions. |
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Parise, Cláudia KloseCalliari, Lauro JúlioKrusche, Nisia2012-11-29T00:27:26Z2012-11-29T00:27:26Z2009PARISE, Cláudia Klose; CALLIARI, Lauro Júlio, KRUSCHE, Nisia. Extreme storm surges in the south of Brazil: atmospheric conditions and shore erosion. Brazilian Journal of Oceanography, v. 57, n. 3, p. 175-188, 2009. Disponível em: <http://www.scielo.br/pdf/bjoce/v57n3/v57n3a02.pdf>. Acesso em: 24 jun. 2012.1982-436Xhttp://repositorio.furg.br/handle/1/2865The region under study is regularly subject to the occurrence of storms associated with frontal systems and extratropical cyclones, since it is located near one of the cyclogenetic regions in South America. These storms can generate storm surges that cause anomalous high sea level rises on Cassino Beach. The use of reanalysis data along with an efficient technique for the location of the cyclone, using a vorticity threshold, has provided a new classification based upon the trajectories of events that produce positive sea level variation. Three patterns have been identified: 1) Cyclogenesis to the south of Argentina with displacement to the east and a trajectory between 47.5ºS and 57.5ºS; 2) Cyclogenesis to the south of Uruguay with displacement to the east and a trajectory between 35ºS and 42.5ºS; and 3) Cyclogenesis to the south of Uruguay with displacement to the southeast and a trajectory between 35ºS and 57.5ºS. Maximum water level elevation above the mean sea level and beach erosion were associated, respectively, with winter and summer storms. Cassino beach displayed a seasonal morphological behavior, with short periods of episodic erosion associated with winter storm events followed by long periods of accretion characterized by the dominance of fair weather conditions.Marés meteorológicas que geram sobre elevações do nível do mar são freqüentes na costa do Rio Grande do Sul e respondem às variações ocorridas na atmosfera. Torna-se importante, dessa maneira, definir padrões meteorológicos sinóticos responsáveis por gerar eventos de marés meteorológicas intensas na Praia do Cassino como objetivo desse trabalho. O uso de dados de reanálise associados a uma técnica eficiente de localização do ciclone, aplicando o conceito de vorticidade, permitiu definir uma nova classificação com base na trajetória de ciclones extratropicais responsáveis pela subida do nível do mar. Três padrões de trajetórias foram identificados: 1) Ciclogênese ao sul da Argentina com deslocamento para leste e trajetória entre 47.5ºS e 57.5ºS; 2) Ciclogênese ao sul do Uruguai com deslocamento para leste e trajetória entre 35ºS e 42.5ºS; 3) Ciclogênese ao sul do Uruguai com deslocamento para sudeste e trajetória entre 35ºS e 57.5ºS. O estudo de 23 ciclones extratropicais permitiu verificar máximas elevações do nível e erosão respectivamente associados a tempestades ocorridas no inverno e verão. A Praia do Cassino apresentou um comportamento sazonal, com erosão episódica associada a eventos de alta energia mais freqüentes no inverno, e longos períodos de acresção relacionados ao regime hidrodinâmico normal.engStorm surgeExtratropical cycloneErosionMaré meteorológicaCiclone extratropicalErosãoExtreme storm surges in the south of Brazil: atmospheric conditions and shore erosioninfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleinfo:eu-repo/semantics/openAccessreponame:Repositório Institucional da FURG (RI FURG)instname:Universidade Federal do Rio Grande (FURG)instacron:FURGORIGINALEXTREME STORM SURGES IN THE SOUTH OF BRAZIL.pdfEXTREME STORM SURGES IN THE SOUTH OF BRAZIL.pdfapplication/pdf2578059https://repositorio.furg.br/bitstream/1/2865/1/EXTREME%20STORM%20SURGES%20IN%20THE%20SOUTH%20OF%20BRAZIL.pdf6eb8ba355704b9ef31288058529f23e4MD51open accessLICENSElicense.txtlicense.txttext/plain; charset=utf-81724https://repositorio.furg.br/bitstream/1/2865/2/license.txt5b92b9704b4f13242d70e45ddef35a68MD52open access1/28652022-10-11 15:00:48.688open accessoai:repositorio.furg.br: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Repositório InstitucionalPUBhttps://repositorio.furg.br/oai/request || http://200.19.254.174/oai/requestopendoar:2022-10-11T18:00:48Repositório Institucional da FURG (RI FURG) - Universidade Federal do Rio Grande (FURG)false |
dc.title.pt_BR.fl_str_mv |
Extreme storm surges in the south of Brazil: atmospheric conditions and shore erosion |
title |
Extreme storm surges in the south of Brazil: atmospheric conditions and shore erosion |
spellingShingle |
Extreme storm surges in the south of Brazil: atmospheric conditions and shore erosion Parise, Cláudia Klose Storm surge Extratropical cyclone Erosion Maré meteorológica Ciclone extratropical Erosão |
title_short |
Extreme storm surges in the south of Brazil: atmospheric conditions and shore erosion |
title_full |
Extreme storm surges in the south of Brazil: atmospheric conditions and shore erosion |
title_fullStr |
Extreme storm surges in the south of Brazil: atmospheric conditions and shore erosion |
title_full_unstemmed |
Extreme storm surges in the south of Brazil: atmospheric conditions and shore erosion |
title_sort |
Extreme storm surges in the south of Brazil: atmospheric conditions and shore erosion |
author |
Parise, Cláudia Klose |
author_facet |
Parise, Cláudia Klose Calliari, Lauro Júlio Krusche, Nisia |
author_role |
author |
author2 |
Calliari, Lauro Júlio Krusche, Nisia |
author2_role |
author author |
dc.contributor.author.fl_str_mv |
Parise, Cláudia Klose Calliari, Lauro Júlio Krusche, Nisia |
dc.subject.por.fl_str_mv |
Storm surge Extratropical cyclone Erosion Maré meteorológica Ciclone extratropical Erosão |
topic |
Storm surge Extratropical cyclone Erosion Maré meteorológica Ciclone extratropical Erosão |
description |
The region under study is regularly subject to the occurrence of storms associated with frontal systems and extratropical cyclones, since it is located near one of the cyclogenetic regions in South America. These storms can generate storm surges that cause anomalous high sea level rises on Cassino Beach. The use of reanalysis data along with an efficient technique for the location of the cyclone, using a vorticity threshold, has provided a new classification based upon the trajectories of events that produce positive sea level variation. Three patterns have been identified: 1) Cyclogenesis to the south of Argentina with displacement to the east and a trajectory between 47.5ºS and 57.5ºS; 2) Cyclogenesis to the south of Uruguay with displacement to the east and a trajectory between 35ºS and 42.5ºS; and 3) Cyclogenesis to the south of Uruguay with displacement to the southeast and a trajectory between 35ºS and 57.5ºS. Maximum water level elevation above the mean sea level and beach erosion were associated, respectively, with winter and summer storms. Cassino beach displayed a seasonal morphological behavior, with short periods of episodic erosion associated with winter storm events followed by long periods of accretion characterized by the dominance of fair weather conditions. |
publishDate |
2009 |
dc.date.issued.fl_str_mv |
2009 |
dc.date.accessioned.fl_str_mv |
2012-11-29T00:27:26Z |
dc.date.available.fl_str_mv |
2012-11-29T00:27:26Z |
dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article |
format |
article |
status_str |
publishedVersion |
dc.identifier.citation.fl_str_mv |
PARISE, Cláudia Klose; CALLIARI, Lauro Júlio, KRUSCHE, Nisia. Extreme storm surges in the south of Brazil: atmospheric conditions and shore erosion. Brazilian Journal of Oceanography, v. 57, n. 3, p. 175-188, 2009. Disponível em: <http://www.scielo.br/pdf/bjoce/v57n3/v57n3a02.pdf>. Acesso em: 24 jun. 2012. |
dc.identifier.uri.fl_str_mv |
http://repositorio.furg.br/handle/1/2865 |
dc.identifier.issn.none.fl_str_mv |
1982-436X |
identifier_str_mv |
PARISE, Cláudia Klose; CALLIARI, Lauro Júlio, KRUSCHE, Nisia. Extreme storm surges in the south of Brazil: atmospheric conditions and shore erosion. Brazilian Journal of Oceanography, v. 57, n. 3, p. 175-188, 2009. Disponível em: <http://www.scielo.br/pdf/bjoce/v57n3/v57n3a02.pdf>. Acesso em: 24 jun. 2012. 1982-436X |
url |
http://repositorio.furg.br/handle/1/2865 |
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eng |
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eng |
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info:eu-repo/semantics/openAccess |
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openAccess |
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