[MITgcm-support] diagnosing gmredi fluxes for tracers
Christoph Voelker
christoph.voelker at awi.de
Mon Oct 28 18:34:05 EDT 2013
Dear MITgcm'ers,
I have a run of a biogeochemical model (i.e. with several additional
passive tracers) and I am trying to diagnose (and hopefully understand)
what the GMREDI eddy parameterization contributes to my tracer fluxes.
In doing so I got somewhat confused my the many options and parameter
settings that are possible in that package; I found it hard to follow
how the advective and diffusive fluxes are really calculated.
My settings include
#define GM_VISBECK_VARIABLE_K
#define GM_BOLUS_ADVEC
in GMREDI_OPTIONS.h.
so, I am using the bolus velocity form, not the skew flux form, with
variable kappa_GM, a la Visbeck et al. '97. In addition I am using the
Large, Danabasoglu, Doney tapering scheme.
My questions concern the diagnostics associated with the tracer fluxes.
- Firstly, I assume that the explicit diffusive terms like DFrETr01
contain the Redi isopycnal diffusion, perhaps plus the additional
diffusion induced e.g. by the KPP sheme that I am using. Is this right?
- Secondly, is the bolus advective flux part of the advective flux
diagnostics, like ADVrTr01? Or is this only the non-bolus advection?
- And finally, is there a way to diagnose the advective tracer fluxes
from the bolus velocity alone, i.e. separate it from the background
velocity advection, in a diagnostic variable, or does one have to write
out the bolus stream function terms GM_PsiX and GM_PsiY, and then
compute the induced additional advection offline?
Sorry if my questions are daft, but I really first tried to understand
all this from the code,
Thanks, Christoph
--
Christoph Voelker
Alfred Wegener Institute for Polar and Marine Research
Am Handelshafen 12
27570 Bremerhaven, Germany
e: Christoph.Voelker at awi.de
t: +49 471 4831 1848
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