2016
DOI: 10.20502/rbg.v17i3.844
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Proposta De Compartimentação Em Mesoescala Para O Litoral Do Nordeste Brasileiro

Abstract: Resumo:As propostas de compartimentação costeira do litoral brasileiro trataram, desde a sistematização dos estudos costeiros no Brasil, o litoral nordestino como uma grande região homogênea do ponto de vista físico-geográfi co. Características como orientação da linha de costa, clima e processos oceanográfi cos conferem a essas duas áreas um quadro paisagístico contrastante, o que levou à investigação e proposição de uma nova compartimentação para o litoral nordestino, feita a partir do desmembramento da porç… Show more

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Cited by 15 publications
(15 citation statements)
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“…The sampling was realized in the framework of the expeditions TAXPOMOL/2016 and Maranhão/2017 in the unexplored part of the northern coast of the north-east region of Brazil, which is named the Brazilian Semi-Arid Coast (Diniz & Oliveira, 2016). All samples were collected in the intertidal zone, on sandy beaches, with rocky tide pools, from the states of Maranhão and Ceará (Figure 1).…”
Section: Methodsmentioning
confidence: 99%
“…The sampling was realized in the framework of the expeditions TAXPOMOL/2016 and Maranhão/2017 in the unexplored part of the northern coast of the north-east region of Brazil, which is named the Brazilian Semi-Arid Coast (Diniz & Oliveira, 2016). All samples were collected in the intertidal zone, on sandy beaches, with rocky tide pools, from the states of Maranhão and Ceará (Figure 1).…”
Section: Methodsmentioning
confidence: 99%
“…Oliveira, 2016), with average height of 1 m and maximum height of 2 m (Frazão and Amaro, 2016). The water depth in the area located seaward from the studied morphology is up to 20 m within a range of 15 km from the coast (Diniz and Oliveira, 2016).…”
Section: Physiography and Geological Frameworkmentioning
confidence: 91%
“…Martin et al, 1993). The local winds come from NE, SE and E directions, with annual speed ranging from 3 to 6 m/s (Diniz and Oliveira, 2016;Frazão and Amaro, 2016). The waves move preferentially in the ESE direction, reaching the coast at right angles (Diniz and Rossetti et al, 2012).…”
Section: Physiography and Geological Frameworkmentioning
confidence: 99%
“…Por conseguinte, foram definidas as unidades morfoesculturais, como segundo nível taxonômico, e as subunidades morfoesculturais, no terceiro nível, sendo este último nível, delimitado com base em Diniz et al (2016). Por fim tornou-se possível delimitar os modelados, que compões o quarto nível taxonômico.…”
Section: Procedimento Metodológicosunclassified