Fluids Group Seminar

Tue, Aug 14, 2018, 11:00 am to 12:00 pm

Current visions and modelling of stratified geophysical turbulence are to a large extent based on the conventional paradigm, leaving no alternative to the downgradient turbulent transports (quantified via turbulent viscosity, heat conductivity and diffusivity) and the forward cascades of kinetic energy and other properties of turbulence – towards molecular dissipations. These concepts underlie turbulence-closure models, theory/modelling of turbulent diffusion, and Monin-Obukhov Similarity Theory (MOST) of the surface-layer turbulence. In this framework, turbulence in super-critically stable stratifications typical of free atmosphere andocean thermocline is considered as principally the same as in sub-critically stable boundary layers, but just weak due to strong static stability and weak velocity shears. In unstable stratification, convective turbulence generated by buoyancy forces is considered as principally the same as mechanical turbulence generated by mean velocity shears and, thus, subjected to the forward cascades. Recent observational evidences have disclosed principal drawbacks of the conventional theory of stratified turbulence and intolerable uncertainties in its modelling. Nevertheless, neither MOST nor traditional turbulence-closure nor turbulent diffusion models are seriously questioned. Their drawbacks root in the commonly recognised paradigm attributed to Kolmogorov (1941a, b; 1942). However, Kolmogorov only considered shear-generated turbulence in neutrally stratified flows, where his major concepts: (i) only forward energy cascade – from larger to smaller eddies, towards dissipation, and (ii) only down-gradient turbulent fluxes, serve as reasonable approximations. Moreover, Kolmogorov was not responsible for the extension of his paradigm to stratified turbulence. This was made by his followers without proof. This talk demonstrates that the conventional paradigm makes a Procrustean bed for the theory of turbulence in bothunstable stratification (Zilitinkevich, 1973, 2013; Zilitinkevich at al., 2006) and strongly stable stratification (Zilitinkevich et al., 2008, 2013). Wehighlight its restrictive nature; demonstrates miscarriages of conventional theory as applied to essentially stratified flows; and outline Energy- and Flux-Budget (EFB) turbulence-energetics and closure theory accounting for non-gradient turbulent fluxes in both stable and unstable stratifications, inverse energy cascade in convective turbulence, and PBL-scale self-organised convective motions generated via inverse cascades.

E-Quad E225

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