Coarse resolution numerical ocean models must typically include a
parameterisation for mesoscale turbulence. A common recipe for such
parameterisations is to invoke down-gradient mixing, or diffusion, of some
tracer quantity, such as potential vorticity or buoyancy. However, it is well
known that eddy fluxes include large rotational components which necessarily do
not lead to any mixing; eddy diffusivities diagnosed from unfiltered fluxes are
thus contaminated by the presence of these rotational components. Here a new
methodology is applied whereby eddy diffusivities are diagnosed directly from
the eddy force function. The eddy force function depends only upon flux
divergences, is independent of any rotational flux components, and is
inherently non-local and smooth. A one-shot inversion procedure is applied,
minimising the mis-match between parameterised force functions and force
functions derived from eddy resolving calculations. This enables diffusivities
associated with the eddy potential vorticity and buoyancy fluxes to be
diagnosed. The methodology is applied to multi-layer quasi-geostrophic ocean
gyre simulations. It is found that: (i) a strictly down-gradient mixing scheme
has limited success in reducing the mis-match compared to one with no sign
constraint on the diffusivity; (ii) negative signals of diffusivities are
prevalent around the time-mean jet; (iii) there is some indication that the
magnitude of the diffusivity correlates well the eddy energy. Implications for
parameterisation are discussed in light of these diagnostic results.Comment: 22 pages, 14 figures, Elsevier template, submitted to Ocean
Modelling; comments welcom