[MITgcm-support] vertical mixing of momentum during convective adjustment
Jody Klymak
jklymak at uvic.ca
Wed Aug 12 00:16:10 EDT 2015
Hi Dimitris…
pkg/kl10 in relatively recent MITgcms does this, though the viscosity is not a constant, its depends on the dissipation inferred from the displacement from its sorted depth dz, and its mean (sorted) stratification N: K = 0.2 dz^2 N. You could easily change that code to just have a constant in unstable regions if you prefer that approach.
Cheers, Jody
> On Aug 11, 2015, at 16:30 PM, Menemenlis, Dimitris (329D) <Dimitris.Menemenlis at jpl.nasa.gov> wrote:
>
> Is there a way to increase viscosity during convective adjustment,
> in the same way that ivdc_kappa increases diffusivity?
>
> That is is there a scheme that includes the following parameters from KPP
> c difmcon = viscosity due to convective instability (m^2/s)
> c difscon = tracer diffusivity .. (m^2/s)
> but without all the other baggage?
>
> Thanks, Dimitris
>
>
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