Statistical optimization for passive scalar transport: maximum entropy production vs maximum Kolmogorov-Sinay entropy
arXiv:1505.06861 · doi:10.5194/npg-22-187-2015
Abstract
We derive rigorous results on the link between the principle of maximum entropy production and the principle of maximum Kolmogorov-Sinai entropy using a Markov model of the passive scalar diffusion called the Zero Range Process. We show analytically that both the entropy production and the Kolmogorov-Sinai entropy seen as functions of f admit a unique maximum denoted fmaxEP and fmaxKS. The behavior of these two maxima is explored as a function of the system disequilibrium and the system resolution N. The main result of this article is that fmaxEP and fmaxKS have the same Taylor expansion at _rst order in the deviation of equilibrium. We find that fmaxEP hardly depends on N whereas fmaxKS depends strongly on N. In particular, for a fixed difference of potential between the reservoirs, fmaxEP (N) tends towards a non-zero value, while fmaxKS (N) tends to 0 when N goes to infinity. For values of N typical of that adopted by Paltridge and climatologists we show that fmaxEP and fmaxKS coincide even far from equilibrium. Finally, we show that one can find an optimal resolution N_ such that fmaxEP and fmaxKS coincide, at least up to a second order parameter proportional to the non-equilibrium uxes imposed to the boundaries.
arXiv commentNonlinear Processes in Geophysics (2015)
References in corpus (7)
- Entropy Rate of Diffusion Processes on Complex Networks
- Localization of maximal entropy random walk
- Condensation in the zero range process: stationary and dynamical properties
- Zero-range process with open boundaries
- Non-equilibrium steady states : maximization of the Shannon entropy associated to the distribution of dynamical trajectories in the presence of constraints
- An optimization principle for deriving nonequilibrium statistical models of Hamiltonian dynamics
- Present and Last Glacial Maximum climates as states of maximum entropy production