Parameterization of eddy fluxes based on a mesoscale energy budget. (August 2015)

• Record Type: Journal Article
• Authors: Jansen, Malte F.; Adcroft, Alistair J.; Hallberg, Robert; Held, Isaac M.
• Is Part Of: Ocean modelling. Volume 92(2015:Aug.)
• Page Start: 28
• Page End: 41
• Publication Date: 2015-08
• Subjects: Eddy parameterization -- Eddy kinetic energy -- Eddy diffusivity -- Mesoscale -- Bottom flow -- Rhines scale; Oceanography -- Periodicals; Océanographie -- Périodiques; Oceanography; Periodicals; 551.46
• DOI: 10.1016/j.ocemod.2015.05.007
• Languages: English
• ISSNs: 1463-5003

Abstract

Highlights: Paper discusses energy-budget-based eddy parameterization. Highlights the importance of mixing length, and eddy kinetic energy (EKE) sink. Mixing length is found to be controlled by Rhines scale. EKE sink is controlled by quadratic bottom friction, in nontrivial way. An improved parameterization for the eddy diffusivity is derived. Abstract: It has recently been proposed to formulate eddy diffusivities in ocean models based on a mesoscale eddy kinetic energy (EKE) budget. Given an appropriate length scale, the mesoscale EKE can be used to estimate an eddy diffusivity based on mixing length theory. This paper discusses some of the open questions associated with the formulation of an EKE budget and mixing length, and proposes an improved energy budget-based parameterization for the mesoscale eddy diffusivity. A series of numerical simulations is performed, using an idealized flat-bottomed β -plane channel configuration with quadratic bottom drag. The results stress the importance of the mixing length formulation, as well as the formulation for the bottom signature of the mesoscale EKE, which is important in determining the rate of EKE dissipation. In the limit of vanishing planetary vorticity gradient, the mixing length is ultimately controlled by bottom drag, though the frictional arrest scale predicted by barotropic turbulence theory needs to be modified to account for the effects of baroclinicity. Any significant planetary vorticity gradient, β, is shown to suppress mixing, and limit the effective mixing length to the Rhines scale. While the EKE remains moderated by bottom friction, the bottom signature of EKE is shown to decrease as the appropriately non-dimensionalized friction increases, which considerably weakens the impact of changes in the bottom friction compared to barotropic turbulence. For moderate changes in the bottom-friction, eddy fluxes are thus reasonably well approximated by the scaling relation proposed by Held and Larichev (1996), which ignores the effect of bottom friction.