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Abstract

Classical Rayleigh-Benard convection occurs when a horizontal fluid layer is heated sufficiently strongly from below. In more recent times, there has been increased interest in structured convection, when the heating that is applied is no longer uniform but rather spatially varying in some way. Here, we examine the effect of structured convection in a fluid layer when both the lower and upper boundaries are heated so that their temperatures fluctuate sinusoidally over a common long length scale offset by some phase

Item Type:	Article
Authors/Creators:	Floryan, JM and Hossain, MZ and Bassom, AP
Keywords:	distributed heating, secondary flow, long wavelength modes, convection, long wavelength heating
Journal or Publication Title:	Theoretical and Computational Fluid Dynamics
Publisher:	Springer-Verlag
ISSN:	0935-4964
DOI / ID Number:	10.1007/s00162-018-0482-0
Copyright Information:	Copyright 2019 Springer-Verlag GmbH Germany, part of Springer Nature
Related URLs:	Google Scholar: Bassom, AP
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