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An exact finite-state representation of viscoelastic memory for accelerated sea-level modeling: SLEvolve v1.0
Glacial Isostatic Adjustment (GIA) models solve the gravitationally self-consistent sea-level equation for the response of the solid Earth and the oceans to changing ice loads. As these models are increasingly embedded in coupled ice-sheet simulations, glacial-cycle calculations, and large ensembles
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