Deriva Litorânea ao Longo da Costa do Cacau, Bahia: Repercussões na Geomorfologia Costeira

Littoral drift along the Costa do Cacau, Bahia: repercussions in the coastal geomorphology

dc.contributorpt-BR
dc.contributoren-US
dc.creatorDO NASCIMENTO, LUCAS
dc.creatorBITTENCOURT, ABÍLIO
dc.creatorSANTOS, ADEYLAN
dc.creatorDOMINGUEZ, JOSÉ
dc.date2007-12-31
dc.date.accessioned2018-11-07T21:58:38Z
dc.date.available2018-11-07T21:58:38Z
dc.identifierhttps://seer.ufrgs.br/PesquisasemGeociencias/article/view/19471
dc.identifier10.22456/1807-9806.19471
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/2192280
dc.descriptionIn this study the patterns of sediment dispersion along part of the southern coast of Bahia, known as the Cacao Coast, were defined, starting with a numerical modeling on wave refraction diagrams. These patterns are able to reproduce net longshore drift direction of sediments in sections where there are geomorphic evidences of the longshore drift direction, and also reasonably explain the different coastal sections under deposition and erosion or little/no deposition, identified by walking the entire extension of the area under study. In a general way, the Cacao Coast may be divided into two sectors with well-defined characteristics: a) the northern half, with a predominance of sections under erosion or little/no deposition, and b) the southern half, with a predominance of sections under deposition.pt-BR
dc.descriptionIn this study the patterns of sediment dispersion along part of the southern coast of Bahia, known as the Cacao Coast, were defined, starting with a numerical modeling on wave refraction diagrams. These patterns are able to reproduce net longshore drift direction of sediments in sections where there are geomorphic evidences of the longshore drift direction, and also reasonably explain the different coastal sections under deposition and erosion or little/no deposition, identified by walking the entire extension of the area under study. In a general way, the Cacao Coast may be divided into two sectors with well-defined characteristics: a) the northern half, with a predominance of sections under erosion or little/no deposition, and b) the southern half, with a predominance of sections under deposition.en-US
dc.formatapplication/pdf
dc.languagepor
dc.publisherInstituto de Geociências /Universidade Federal do Rio Grande do Sulpt-BR
dc.relationhttps://seer.ufrgs.br/PesquisasemGeociencias/article/view/19471/pdf
dc.sourcePesquisas em Geociências; v. 34, n. 2 (2007): Pesquisas em Geociências; 45-56pt-BR
dc.source1807-9806
dc.source1518-2398
dc.subjectpt-BR
dc.subjectpt-BR
dc.subjectGeociênciaspt-BR
dc.subjecten-US
dc.subjectlongshore drift; wave refraction; erosion and deposition sections.en-US
dc.titleDeriva Litorânea ao Longo da Costa do Cacau, Bahia: Repercussões na Geomorfologia Costeirapt-BR
dc.titleLittoral drift along the Costa do Cacau, Bahia: repercussions in the coastal geomorphologyen-US
dc.typeArtículos de revistas
dc.typeArtículos de revistas
dc.coverageBahia;Brasilpt-BR
dc.coveragept-BR
dc.coveragept-BR


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