Reference health

Stability transitions and turbulence in horizontal convection

https://doi.org/10.1017/jfm.2014.302
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38/38 checkable references clean · checked 2026-07-23

Every reference with a DOI in the deposited reference list resolved to a known work in Crossref or DataCite at the dated check, and none carried a retraction, withdrawal, or removal notice.

2 without a DOI — not checked. A reference deposited without a DOI is never matched by title or guessed at; it stays outside the checked set, and this line discloses that.

The 38 checked references that resolve
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Horizontal convection is non-turbulent
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Mixing in stratified fluids
resolves10.1017/jfm.2012.592
Energetics of horizontal convection
resolves10.1146/annurev.fluid.40.111406.102148
Horizontal Convection
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The wind in confined thermal convection
resolves10.1017/S0022112007005630
A theoretical model for horizontal convection at high Rayleigh number
resolves10.1103/RevModPhys.81.503
Heat transfer and large scale dynamics in turbulent Rayleigh-Bénard convection
resolves10.1017/jfm.2011.170
Direct and large-eddy simulations of internal tide generation at a near-critical slope
resolves10.1029/2008JC005152
Effects of topography on the cumulative mixing efficiency in exchange flows
resolves10.1017/S0022112009006685
Available potential energy and buoyancy variance in horizontal convection
resolves10.1017/S0022112009992461
Radial boundary layer structure and Nusselt number in Rayleigh–Bénard convection
resolves10.1017/S002211200999111X
On the energetics of stratified turbulent mixing, irreversible thermodynamics, Boussinesq models and the ocean heat engine controversy
resolves10.1017/S0022112094004465
Three-dimensional wave instability near a critical level
resolves10.1017/S002211209500125X
Available potential energy and mixing in density-stratified fluids
resolves10.1017/S002211200999200X
Large eddy simulation of a stratified boundary layer under an oscillatory current
resolves10.1017/S0022112008002942
Very viscous horizontal convection
resolves10.1017/S0022112002007851
An investigation of stably stratified turbulent channel flow using large-eddy simulation
resolves10.1016/S0377-0265(99)00025-1
Turbulent mixing in a stratified fluid
resolves10.1103/PhysRevLett.107.174503
Local Energy Dissipation Rate Balances Local Heat Flux in the Center of Turbulent Thermal Convection
resolves10.1017/jfm.2013.244
Horizontal convection dynamics: insights from transient adjustment
resolves10.1017/S0022112097005429
Large-eddy simulation of the turbulent mixing layer
resolves10.3402/tellusa.v50i2.14523
Numerical experiments with a fluid heated non-uniformly from below
resolves10.1017/S0022112004000485
Convection driven by differential heating at a horizontal boundary
resolves10.1029/2011GL049701
Is horizontal convection really “non-turbulent?”
resolves10.1088/1367-2630/12/7/075022
Boundary layer structure in turbulent thermal convection and its consequences for the required numerical resolution
resolves10.1175/2009JPO4162.1
Available Potential Energy and Irreversible Mixing in the Meridional Overturning Circulation
resolves10.7551/mitpress/3014.001.0001
A First Course in Turbulence
resolves10.1017/jfm.2013.136
Rotating horizontal convection
resolves10.1103/PhysRevLett.111.124301
Completing the Mechanical Energy Pathways in Turbulent Rayleigh-Bénard Convection
resolves10.1017/S0022112008000554
Mixing efficiency in controlled exchange flows
resolves10.1029/2011JC006980
When do marginal seas and topographic sills modify the ocean density structure?
resolves10.1103/PhysRevLett.104.218502
Turbulence During the Generation of Internal Tide on a Critical Slope
resolves10.1063/1.857955
A dynamic subgrid-scale eddy viscosity model
resolves10.1017/jfm.2013.353
Available potential energy in Rayleigh–Bénard convection
resolves10.1073/pnas.48.5.766
ON THE SMALLNESS OF SINKING REGIONS IN THE OCEAN
resolves10.1063/1.858675
A dynamic mixed subgrid-scale model and its application to turbulent recirculating flows
resolves10.1016/j.ocemod.2005.04.001
A simple convective model of the global overturning circulation, including effects of entrainment into sinking regions
resolves10.1146/annurev.fluid.35.101101.161144
M<scp>IXING</scp> E<scp>FFICIENCY IN</scp> S<scp>TRATIFIED</scp> S<scp>HEAR</scp> F<scp>LOWS</scp>
The 2 references without a DOI — listed, not checked
no DOI — not checkedOn thermal convection driven by non-uniform heating from below: an experimental study
no DOI — not checkedLund, T. S. 1997 On the use of discrete filters for large eddy simulation. In Annual Research Briefs, pp. 83–95. Centre for Turbulence Research, NASA Ames–Stanford University.
What this badge says. CiteStamped means the CHECKABLE references of this work were clean at the dated check: each resolved to a known work in a public registry, and none carried a retraction notice at that time. It says nothing about the quality, findings, or importance of the work itself, and nothing about references deposited without a DOI.

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