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Volume 15, Issue 3 - September 2015

 

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Revista de Gestão Costeira Integrada
Volume 15, Número 3, Setembro 2015, Páginas 353-370

DOI: 10.5894/rgci570
* Submission: 21 DEC 2014; Peer review: 17 JAN 2015; Revised: 9 MAR 2015; Accepted: 28 MAR 2015; Available on-line: 30 MAR 2015  

Supporting Information (561KB, PDF)

Analysis of the influence of ENSO phenomena on wave climate on the central coastal zone of Rio de Janeiro (Brazil) *  

Nair Emmanuela da Silveira Pereira@, a; Leonardo Azevedo Klumb-Oliveirab


@ - Corresponding author, to whom correspondence should be addressed: a - MAG - Mar, Ambiente e Geologia – Serviços. Rua Visconde de Inhaúma, 37 - 21º andar, Centro, CEP: 20091-007, Rio de Janeiro, RJ, Brazil. e-mail: Pereira <[email protected]>
b - Universidade Federal do Rio de Janeiro - Programa de Pós-Graduação em Geografia. Avenida Athos da Silveira Ramos, 274 - Prédio do CCMN - Bloco I - Cidade Universitária, CEP: 21.941-916, Rio de Janeiro, RJ, Brazil. e-mail: Klumb-Oliveira <[email protected]>


ABSTRACT
This paper evaluates the influence of the El Niño – Southern Oscillation on the wave climate variability in the central region of Rio de Janeiro’s coastal zone. The regional climate of the area was characterized using the WAVEWATCH III wave data model, obtained from NOAA, organized as a 35 year time series (1979-2013). These data were validated for the study area and a characterization and analysis performed by focusing on years with occurrence of strong El Niño/La Niña events. The correlation between the interannual variability of significant wave height and Oceanic Niño Index showed a slight reduction in significant wave height during El Niño years and the opposite pattern during La Niña years, with a lag of four months. This decrease could be attributed to the intensification of the South Atlantic High with a corresponding increase in the occurrence of subtropical jets during periods of El Niño. This weather change causes the blocking of cold fronts in the southern region of Brazil and the consequent reduction in the percentage of waves from the south along the southeast coast.

Palavras-chave: climate variability, wave parameters, interannual time scale, seasonality, regional climatology.   


Análise da influência de fenômenos ENOS no clima de ondas da porção central da zona costeira do Rio de Janeiro (Brasil)

RESUMO
Este artigo busca avaliar a influência do fenômeno El Niño - Oscilação Sul na variabilidade do clima de ondas da porção central da zona costeira do Rio de Janeiro. Para tanto, a climatologia regional da área foi caracterizada a partir de dados de ondas do modelo WAVEWATCH III disponibilizado pela NOAA, organizados numa série temporal de 35 anos (1979 - 2013). Esses dados foram validados para a área de estudo e, realizada sua caracterização e análise com enfoque em anos de acentuada ocorrência
de eventos de El Niño/La Ninã. A correlação da variabilidade interanual da série de altura significativa de ondas e Índice de Niño Oceânico mostrou padrão de leve redução das alturas significativas em anos de El Niño e, o inverso para anos de La Niña, com defasagem temporal de quatro meses na região. Essa redução na altura significativa das ondas pode ser atribuída à intensificação da Alta Subtropical do Atlântico Sul e aumento na ocorrência de jatos subtropicais nos períodos de El Niño. Essa alteração no padrão meteorológico causa o bloqueio de frentes frias na região Sul do Brasil e consequente redução da porcentagem de ondas de sul na região sudeste.    
Keywords: GIS, coastal management, mariculture, cobia, Rachycentron canadum. 

 

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