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The model computes flow accumulation using multiple flow direction over unstructured grids based on an adaptation of the implicit approach proposed by Richardson et al. (Richardson, Hill, & Perron, 2014). An extension of the parallel priority-flood depressionfilling algorithm from (Barnes, 2016) to unstructured mesh is used to simulate sedimentation in upland areas and internally drained basins. Marine sedimentation is based on a diffusion algorithm similar to the technique proposed in pybadlands (Salles, Ding, & Brocard, 2018).

eSCAPE: parallel global-scale landscape evolution model