Fluid Motions in the Presence of Strong Stable Stratification

By J. Riley, M. Lelong. 2000

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TOWARD REGIONAL CHARACTERIZATIONS OF THE OCEANIC INTERNAL WAVEFIELD (2010, background): “The dynamics in this limit are those of stratified rotating turbulence in which motions at different isopycnals are uncoupled at scales larger than those over which shear instabilities can develop [Riley and Lelong, 2000].”
Stably Stratified Atmospheric Boundary Layers (2014, background): “Turbulence in stratified flows in laboratory settings and numerical simulations is easier (but still difficult) to understand (Ohya et al. 2008, Riley & Lelong 2000).”
INTERNAL GRAVITY WAVES: From Instabilities to Turbulence (2002, background): “This confirms results obtained directly on triad interactions, without statistical averaging (Riley & Lelong 2000).”
Stratified turbulence dominated by vortical motion (2004, methodology): “Following Riley et al. (1981), we scale Π1 by N (2)U/Lh and B0 by U (2)/Lz.”
Scaling analysis and simulation of strongly stratified turbulent flows (2007, background): “The advection terms involving vertical derivatives in (2.8) and (2.11) can be neglected under these assumptions and the continuity equation (2.10) reduces to ∇h · uh = 0 (Riley et al. 1981; Riley & Lelong 2000).”
Generation of slow large scales in forced rotating stratified turbulence (2002, background): “The reader is referred to the recent review by Riley & Lelong (2000) for further discussion and references on stably stratified flows.”