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.
Vegetation Patterning Can Both Impede and Trigger Critical Transitions from Sa- vanna to Grassland
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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.