Hexaroll chaos in inclined layer convection

dc.creatorBrunner, W.
dc.creatorMcCoy, J.
dc.creatorPesch, W.
dc.creatorBodenschatz, E.
dc.date2006-01-05
dc.date.accessioned2026-07-07T06:59:34Z
dc.date.available2026-07-07T06:59:34Z
dc.descriptionWe report experimental observations of hexaroll chaos in inclined layer convection. Two separate populations of defect complexes characterize the defect turbulent state, one the classical penta-hepta defect of hexagonal planform patterns, and the other a short-lived complex capable of self-annihilation. By measuring the defect statistics we show that short-lived defect complexes give rise to linear defect destruction rates. This observation explains previous results in other defect-turbulent pattern forming systems.
dc.description4 pages, 5 figures, to be submitted to PRL
dc.identifierhttps://arxiv.org/abs/nlin/0601016
dc.identifierhttp://arxiv.org/abs/nlin/0601016
dc.identifier.urihttp://salesiana.dossiersoluciones.com/handle/123456789/107793
dc.subjectPattern Formation and Solitons
dc.titleHexaroll chaos in inclined layer convection
dc.typetext

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