Fractality of eroded coastlines of correlated landscapes
Pablo A. Morais, Erneson A. Oliveira, Nuno A. M. Araujo, H. J., Herrmann, J. S. Andrade Jr

TL;DR
This study uses numerical simulations to explore how spatial correlations in landscapes influence the fractal nature of coastlines, revealing a continuous variation in fractal dimensions linked to landscape correlations.
Contribution
It demonstrates that landscape correlations affect coastline fractality, showing a nonuniversal behavior consistent with real-world coastlines, and connects erosion dynamics to percolation and universality classes.
Findings
Fractal dimension at critical erosion is D=1.33 for uncorrelated landscapes.
Above critical force, coastlines are self-affine in the KPZ class.
Fractal dimension varies with Hurst exponent in correlated landscapes.
Abstract
Using numerical simulations of a simple sea-coast mechanical erosion model, we investigate the effect of spatial long-range correlations in the lithology of coastal landscapes on the fractal behavior of the corresponding coastlines. In the model, the resistance of a coast section to erosion depends on the local lithology configuration as well as on the number of neighboring sea sides. For weak sea forces, the sea is trapped by the coastline and the eroding process stops after some time. For strong sea forces erosion is perpetual. The transition between these two regimes takes place at a critical sea force, characterized by a fractal coastline front. For uncorrelated landscapes, we obtain, at the critical value, a fractal dimension D=1.33, which is consistent with the dimension of the accessible external perimeter of the spanning cluster in two-dimensional percolation. For sea forces…
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