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Kinetic energy cascade in stably stratified open-channel flows
by
Atoufi, Amir
, Scott, K. Andrea
, Waite, Michael L.
in
Atmospheric boundary layer
/ Budgets
/ Buffer layers
/ Channel flow
/ Computational fluid dynamics
/ Density
/ Energy
/ Energy spectra
/ Fluid mechanics
/ Flux density
/ Height
/ JFM Papers
/ Kinetic energy
/ Open channel flow
/ Stratification
/ Turbulence
/ Velocity
/ Viscous sublayers
2021
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Kinetic energy cascade in stably stratified open-channel flows
by
Atoufi, Amir
, Scott, K. Andrea
, Waite, Michael L.
in
Atmospheric boundary layer
/ Budgets
/ Buffer layers
/ Channel flow
/ Computational fluid dynamics
/ Density
/ Energy
/ Energy spectra
/ Fluid mechanics
/ Flux density
/ Height
/ JFM Papers
/ Kinetic energy
/ Open channel flow
/ Stratification
/ Turbulence
/ Velocity
/ Viscous sublayers
2021
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While trying to remove the title from your shelf something went wrong :( Kindly try again later!
Do you wish to request the book?
Kinetic energy cascade in stably stratified open-channel flows
by
Atoufi, Amir
, Scott, K. Andrea
, Waite, Michael L.
in
Atmospheric boundary layer
/ Budgets
/ Buffer layers
/ Channel flow
/ Computational fluid dynamics
/ Density
/ Energy
/ Energy spectra
/ Fluid mechanics
/ Flux density
/ Height
/ JFM Papers
/ Kinetic energy
/ Open channel flow
/ Stratification
/ Turbulence
/ Velocity
/ Viscous sublayers
2021
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Kinetic energy cascade in stably stratified open-channel flows
Journal Article
Kinetic energy cascade in stably stratified open-channel flows
2021
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Overview
In this paper, the kinetic energy cascade in stably stratified open-channel flows is investigated. A mathematical framework to incorporate vertical scales into the conventional kinetic energy spectrum and its budget is introduced. This framework defines kinetic energy density in horizontal spectral and vertical scale space. The energy cascade is studied by analysing the evolution of kinetic energy density. It is shown that energetic streamwise scales ($\\lambda _x$) become larger with increasing vertical scale. For the strongest stratification, for which the turbulence becomes intermittent, the energetic streamwise scales are suppressed, and energy density resides in $\\lambda _x$ of the size of the domain. It is shown that, in an unstratified case, vertical scales of the size comparable to the height of the logarithmic layer connect viscous regions to the outer layer. By contrast, in stratified cases, such a connection is not observed. Moreover, it is shown that nonlinear transfer for streamwise scales is dominated by in-plane triad interactions and inter-plane transfer is more active in transferring energy density among small vertical scales of the size comparable to the height of viscous sublayer. The vertical scales of size comparable to the height of the viscous sublayer and buffer layer are the most active scales in the viscous term and the production term in the energy density budget, respectively.
Publisher
Cambridge University Press
Subject
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