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A quasi-normal scale elimination model of turbulence and its application to stably stratified flows
quasi-normal scale elimination model turbulence application stably stratified flows
2009/11/9
Models of planetary, atmospheric and oceanic circulation involve eddy viscosity and eddy diffusivity, KM and KH, that account for unresolved turbulent mixing and diffusion. The most sophisticated turb...
A Comparison of Length Scales and Decay Times of Turbulence in Stably Stratified Flows
Length Scales Decay Times Stably Stratified Flows
2009/1/13
An examination of average values of a buoyancy length scale, LR = (/N3)½, and a Thorpe scale, LT, computed from vertical profiles of oceanic turbulence at 150°W in the tropical Pacific Ocean, s...
The Wave–Turbulence Transition for Stratified Flows
Wave–Turbulence Transition Stratified Flows
2008/7/1
Mixing in a stratified ocean is controlled by different physics, depending on the large-scale Richardson number. At high Richardson numbers, mixing is controlled by interactions between internal wave ...
Lagrangian Measurements of Waves and Turbulence in Stratified Flows
Lagrangian Measurements Waves Turbulence Stratified Flows
2008/6/30
Stratified flows are often a mixture of waves and turbulence. Here, Lagrangian frequency is used to distinguish these two types of motion.
A set of 52 Lagrangian float trajectories from Knight Inlet ...