Please use this identifier to cite or link to this item: http://hdl.handle.net/11422/8821
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dc.contributor.authorLoureiro, Juliana Braga Rodrigues-
dc.contributor.authorMonteiro, André Sampaio-
dc.contributor.authorPinho, Fernando Manuel Coutinho Tavares de-
dc.contributor.authorFreire, Atila Pantaleão Silva-
dc.date.accessioned2019-07-16T15:17:56Z-
dc.date.available2023-12-21T03:01:25Z-
dc.date.issued2008-09-30-
dc.identifier.issn0006-8314pt_BR
dc.identifier.urihttp://hdl.handle.net/11422/8821-
dc.description.abstractThe present work investigates the lower boundary condition for flows over a steep, rough hill. Simple asymptotic arguments together with the mixing-length hypothesis are used to derive a local analytical solution that is tested against three different flow conditions. In all, 36 velocity profiles are compared with the proposed expression. The experiments were carried out in a water channel and velocity measurements were made through laser Doppler anemometry. The extent of separated flow was made to vary as a function of the roughness and the Reynolds number. The analysis includes regions of attached as well as separated flow. In particular, the solution of Stratford is studied at the points of separation and re-attachment and found to apply equally well in rough walls.en
dc.languageengpt_BR
dc.publisherSpringeren
dc.relation.ispartofBoundary-Layer Meteorologyen
dc.rightsAcesso Abertopt_BR
dc.subjectHillen
dc.subjectLaw of the wallen
dc.subjectRoughnessen
dc.subjectSeparationen
dc.titleWater-Tank Studies of Separating Flow Over Rough Hillsen
dc.typeArtigopt_BR
dc.identifier.doi10.1007/s10546-008-9314-xpt_BR
dc.description.resumoIndisponível.pt_BR
dc.publisher.countryBrasilpt_BR
dc.publisher.departmentNúcleo Interdisciplinar de Dinâmica dos Fluidospt_BR
dc.subject.cnpqCNPQ::CIENCIAS EXATAS E DA TERRA::FISICA::AREAS CLASSICAS DE FENOMENOLOGIA E SUAS APLICACOES::DINAMICA DOS FLUIDOSpt_BR
dc.citation.volume129pt_BR
dc.citation.issue2pt_BR
dc.citation.spage289pt_BR
dc.citation.epage308pt_BR
dc.embargo.terms365 diaspt_BR
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