Applicaiton of CROCO to small bays or estuaries


Does anyone have experiences in applications of CROCO to very small areas that are mainly dominated by density-driven currents? For example small and shallow lagoons, bays, estuaries?

Particularly, I am interested in examples where horizontal extent of the domain is up to a few kms (1-2km) and average depths of a few meters (3-6m).

If yes, did CROCO perform well in these applications? Any (publication) reports on it, or hands-on experiences?

Thank you in advance!

I don’t think there is much on that since it would require non-hydrostatic simulations (and wet-dry cells), which is relatively new in CROCO.