Fractional Vegetation-Water Model in Arid and Semi-Arid Environments: Pattern Formation and Numerical Simulations

TL;DR

This paper introduces a fractional mathematical model for vegetation-water dynamics in arid environments, linking slope effects to anomalous water advection and demonstrating pattern formation through numerical simulations.

Contribution

It develops a novel fractional model connecting existing vegetation-water models, incorporating slope effects via the fractional parameter, and analyzes stability and pattern formation.

Findings

Fractional parameter correlates with domain slope and migration speed.

Oscillatory solutions demonstrate vegetation pattern formation.

Model validation confirms the effectiveness of fractional calculus in this context.

Abstract

In this paper, we present a new fractional mathematical model to describe the dynamics and the interaction between plants and water in arid and semi-arid environments with and without slope. By the Caputo fractional operator, the model allows for simulating the phenomena related to the vegetation migration, which occur in domains with different slopes. By assuming the fractional parameter linked to the slope of the domain, the new fractional model represents a connection between the Klausmeier model, where water advection occurs, to the Klausmeier-Gray-Scott model, where water diffuses. The proposed model describes an anomalous physical phenomenon that changes as the fractional parameter changes, modelling an anomalous water advection. An analytical study of the stability of the Hopf bifurcation demonstrates that the migration speed results to be a function of the fractional parameter, confirming the connection between the fractional parameter and the slope of the domain. The oscillatory solutions and the vegetation pattern formation, obtained numerically, validate the analytical results and confirm the reliability and efficiency of the fractional formulation of the considered model.