Scaling in erosion of landscapes: Renormalization group analysis of a model with turbulent mixing
N. V. Antonov, P. I. Kakin

TL;DR
This paper applies renormalization group analysis to a landscape erosion model with turbulent mixing, revealing complex fixed point structures and potential scaling behavior in the infrared range.
Contribution
It extends the landscape erosion model by incorporating anisotropic turbulent advection and derives the full set of renormalization constants and critical exponents.
Findings
Existence of two fixed point surfaces with possible infrared attraction
Model exhibits nonuniversal critical exponents depending on fixed point coordinates
Derivation of one-loop counterterms and renormalization group functions
Abstract
The model of landscape erosion, introduced in [{\it Phys. Rev. Lett.} {\bf 80}: 4349 (1998); {\it J. Stat. Phys.} {\bf 93}: 477 (1998)] and modified in [{\it Theor. Math. Phys.} - in press; arXiv:1602.00432], is advected by anisotropic velocity field. The field is Gaussian with vanishing correlation time and the pair correlation function of the form , where and is the component of the wave vector, perpendicular to a certain preferred direction -- the -dimensional generalization of the ensemble introduced by Avellaneda and Majda [{\it Commun. Math. Phys.} {\bf 131}: 381 (1990)]. Analogous to the case without advection, the model is multiplicatively renormalizable and has infinitely many coupling constants. The one-loop counterterm is derived in a closed form in terms of the certain function ,…
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