2014
DOI: 10.1590/0102-778620130605
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Modelos acoplados do IPCC-AR4 e o gradiente meridional de temperatura da superfície do mar no Atlântico Tropical: relações com a precipitação no norte do nordeste do Brasil

Abstract: International audienc

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Cited by 4 publications
(2 citation statements)
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“…These include areas of low altitude juxtaposed with high declivity, elevated population density, concentrations of both intensely verticalized zones mostly covered by impermeable surfaces, and informal urban settlements inhabited by socially vulnerable populations. It is a city characterized by contrasts that are reflected and interacted with by the climate, leading it to be recognized as one of the most vulnerable cities to climate change worldwide [2].…”
Section: Introductionmentioning
confidence: 99%
“…These include areas of low altitude juxtaposed with high declivity, elevated population density, concentrations of both intensely verticalized zones mostly covered by impermeable surfaces, and informal urban settlements inhabited by socially vulnerable populations. It is a city characterized by contrasts that are reflected and interacted with by the climate, leading it to be recognized as one of the most vulnerable cities to climate change worldwide [2].…”
Section: Introductionmentioning
confidence: 99%
“…Aplicação do modelo auto regressivo vetorial (VAR) para o GMAT e respectivos lag's em grupos homogêneos (GH) das BH Alto Iguaçu (AI), Litorânea (L) e Ribeira (R) -Paraná. GMAT e a as anomalias pluviais na BH Litorânea, descontruindo a hipótese de que este indicador climático, que representa a anomalia TSM do Oceano Atlântico uma das mais representativas e estudadas teleconexões para a ocorrência das anomalias pluviométricas em outras regiões brasileiras(DIAZ;STUDZINSKI, 1994;ALVES et al, 2014;, em certo modo e intensidade exerceria uma influência nas anomalias pluviais na bacia hidrográfica do Litoral paranaense. Demonstra-se que os GH's II e III da BH do rio Ribeira correspondem aos setores de maior influência do indicador climático ODP para a ocorrência das anomalias pluviais para a defasagem temporal de 2 e 3 meses.…”
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