In finite, anisotropic dryland models, periodic vegetation patterns increase susceptibility to nonlinear convective instabilities that drive desertification, contrary to predictions from isotropic infinite-domain models.
Integrating theory and experiments to link local mechanisms and ecosystem-level consequences of vegetation patterns in drylands
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How spatial patterns can lead to less resilient ecosystems
In finite, anisotropic dryland models, periodic vegetation patterns increase susceptibility to nonlinear convective instabilities that drive desertification, contrary to predictions from isotropic infinite-domain models.