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Parallel confined-unconfined aquifer system (CUAS) model (CUAS-MPI)

This code simulates the subglacial hydrological system as an equivalent porous medium, with an evolving transmissivity. High transmissivity represents channelised flow, while low transmissivity represents distributed water flow.


A parallel implementation of the confined–unconfined aquifer system model for subglacial hydrology: design, verification, and performance analysis (CUAS-MPI v0.1.0)

Fischler Y, Kleiner T, Bischof C, Schmiedel J, Sayag R, Emunds R, Oestreich L, Humbert A - Geoscientific Model Development - 2023

Subglacial hydrology

Helmholtz Imaging spinning wheel

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