A boundary-value problem for the parameterized mesoscale eddy transport

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Using a resolution function to regulate parameterizations of oceanic mesoscale eddy effects (2013, background): “, 2009), but this is a misnomer derived from flat-bottom or reduced gravity models; with variable bottom topography a literal interpretation of the isopycnal height diffusivity as a thickness diffusivity leads to a substantial near-bottom source of available potential energy, and this interpretation”
OMIP contribution to CMIP6: experimental and diagnostic protocol for the physical component of the Ocean Model Intercomparison Project (2016, unknown): “(1995) or related methods such as Ferrari et al. (2010).”
The GFDL Global Ocean and Sea Ice Model OM4.0: Model Description and Simulation Features (2019, methodology): “The first is the relaxation of baroclinicity to remove available potential energy from the large scale, for which we follow the ideas of Gent et al. (1995) as implemented using the stream function formulation of Ferrari et al. (2010).”