2017
DOI: 10.1017/jfm.2017.761
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Energy dissipation rate limits for flow through rough channels and tidal flow across topography – CORRIGENDUM

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“…In particular, under the assumption that the profile h (which may differ at the top and bottom boundaries) is a continuous and piecewise differentiable function of the horizontal coordinates and has squared-integrable gradients, the authors showed Nu C( ∇h 2 2 )Ra 1 2 . Here we want to cite also [Ker16] and [Ker18], where Kerswell derives an upper bound for the energy dissipation rate per unit mass for a pressure-driven flow in a rough channel.…”
Section: Introductionmentioning
confidence: 99%
“…In particular, under the assumption that the profile h (which may differ at the top and bottom boundaries) is a continuous and piecewise differentiable function of the horizontal coordinates and has squared-integrable gradients, the authors showed Nu C( ∇h 2 2 )Ra 1 2 . Here we want to cite also [Ker16] and [Ker18], where Kerswell derives an upper bound for the energy dissipation rate per unit mass for a pressure-driven flow in a rough channel.…”
Section: Introductionmentioning
confidence: 99%