2-DIMENSIONAL CONVECTION IN A HORIZONTAL FLUID LAYER WITH SPATIALLY PERIODIC BOUNDARY TEMPERATURES

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dc.contributor.authorYOO, JSko
dc.contributor.authorKim, Moon Uhnko
dc.date.accessioned2013-02-25T03:20:23Z-
dc.date.available2013-02-25T03:20:23Z-
dc.date.created2012-02-06-
dc.date.created2012-02-06-
dc.date.issued1991-06-
dc.identifier.citationFLUID DYNAMICS RESEARCH, v.7, no.3-4, pp.181 - 200-
dc.identifier.issn0169-5983-
dc.identifier.urihttp://hdl.handle.net/10203/59428-
dc.description.abstractTwo-dimensional thermal convection in a fluid layer confined between two horizontal rigid walls kept at spatially periodic temperatures is investigated by direct numerical simulations. With increasing the Rayleigh number, convection evolves from a steady state to a temporally chaotic flow. It is observed that the transition to the chaos occurs via quasi-periodic states with two or three basic frequencies or via sequences of period-doubling bifurcations, according to the boundary temperature distributions.-
dc.languageEnglish-
dc.publisherELSEVIER SCIENCE BV-
dc.title2-DIMENSIONAL CONVECTION IN A HORIZONTAL FLUID LAYER WITH SPATIALLY PERIODIC BOUNDARY TEMPERATURES-
dc.typeArticle-
dc.identifier.wosidA1991FW40300007-
dc.identifier.scopusid2-s2.0-0026170286-
dc.type.rimsART-
dc.citation.volume7-
dc.citation.issue3-4-
dc.citation.beginningpage181-
dc.citation.endingpage200-
dc.citation.publicationnameFLUID DYNAMICS RESEARCH-
dc.identifier.doi10.1016/0169-5983(91)90057-P-
dc.contributor.localauthorKim, Moon Uhn-
dc.contributor.nonIdAuthorYOO, JS-
dc.type.journalArticleArticle-
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