Eddy-mixing entropy and its maximization in forced-dissipative geostrophic turbulence
An equilibrium, or maximum entropy, statistical mechanics theory can be derived for ideal, unforced and inviscid, geophysical flows. However, for all geophysical flows which occur in nature,forcing and dissipation play a major role. Here, a study of eddy-mixing entropy in a forced dissipative barotr...
Hlavní autoři: | David, T, Zanna, L, Marshall, D |
---|---|
Médium: | Journal article |
Vydáno: |
IOP Publishing
2018
|
Podobné jednotky
-
A conjecture on the role of bottom-enhanced diapycnal mixing in the parameterization of geostrophic eddies
Autor: Marshall, D, a další
Vydáno: (2008) -
A regime diagram for ocean geostrophic turbulence
Autor: Klocker, A, a další
Vydáno: (2016) -
Equilibration of an atmosphere by geostrophic turbulence
Autor: Jansen, Malte F. (Malte Friedrich)
Vydáno: (2013) -
Interactions between geostrophic eddies and the mean circulation over large-scale bottom topography
Autor: Adcock, S, a další
Vydáno: (2000) -
DNS of Structural Vacillation in the transition to geostrophic turbulence
Autor: Früh, W, a další
Vydáno: (2007)