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Towards Data-Driven Dynamic Surrogate Models for Ocean Flow
2019
Proceedings of the Platform for Advanced Scientific Computing Conference on - PASC '19
Coarse graining of (geophysical) flow problems is a necessity brought upon us by the wide range of spatial and temporal scales present in these problems, which cannot be all represented on a numerical grid without an inordinate amount of computational resources. Traditionally, the effect of the unresolved eddies is approximated by deterministic closure models, i.e. so-called parameterizations. The effect of the unresolved eddy field enters the resolved-scale equations as a forcing term, denoted
doi:10.1145/3324989.3325713
dblp:conf/pasc/EdelingC19
fatcat:hxtnias2bzdcviq3557srp3cqi