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I've been going through the budget equations to match them with the Langmuir closure Overleaf document and had three of questions/comments:
It looks like the first part of the pressure closure in the u'w' and v'w' budgets is multiplied by an extra factor of a half, as the KE is defined with the factor of half already built in (see below). The factor of half outside makes sense to me, but I'm not sure where the second 0.5 or 0.5_RKIND comes from
I don't follow the flux dissipation terms in the u'v', v'w', u'w', w't', w's'. (which contain kappa_FL or kappa_VAR; I'm also not sure why the latter is defined separate to kappa_FL). I assume these represent the viscous/diffusive terms that have the form $\partial^2(\overline{u'w'})/\partial z^2$, but the numerator looks like a first-order numerical derivative instead of second-order. In the u'w' budget these terms are:
But I think the simplest second-order derivative (assuming that vertical grid spacing is constant) would be kappa_FL*(uw(i1,k-1,iCell) - 2.0_RKIND*uw(i1,k,iCell) + uw(i1,k+1,iCell)) / ( 0.5_RKIND*(ze(k-1,iCell) - ze(k+1,iCell))**2.0_RKIND)
The coefficients for the buoyancy pressure closure change between the different budgets (w'w' contains C2 while all the other budgets contain beta5). Are these connected in your parameter definitions (C2=1-beta5 for energy conservation?), and if so could they be combined for simplicity in the code? It also looks like B could be used to replace the buoyancy flux in the w'w' budget as in the other budgets.
I've been going through the budget equations to match them with the Langmuir closure Overleaf document and had three of questions/comments:
It looks like the first part of the pressure closure in the u'w' and v'w' budgets is multiplied by an extra factor of a half, as the KE is defined with the factor of half already built in (see below). The factor of half outside makes sense to me, but I'm not sure where the second 0.5 or 0.5_RKIND comes from
MPAS-Model/src/core_ocean/shared/mpas_ocn_adcReconstruct.F
Lines 572 to 573 in 4923b0e
MPAS-Model/src/core_ocean/shared/mpas_ocn_adcReconstruct.F
Lines 587 to 588 in 4923b0e
MPAS-Model/src/core_ocean/shared/mpas_ocn_adcReconstruct.F
Lines 498 to 499 in 4923b0e
I don't follow the flux dissipation terms in the u'v', v'w', u'w', w't', w's'. (which contain$\partial^2(\overline{u'w'})/\partial z^2$ , but the numerator looks like a first-order numerical derivative instead of second-order. In the u'w' budget these terms are:
kappa_FLorkappa_VAR; I'm also not sure why the latter is defined separate tokappa_FL). I assume these represent the viscous/diffusive terms that have the formMPAS-Model/src/core_ocean/shared/mpas_ocn_adcReconstruct.F
Lines 580 to 581 in 4923b0e
But I think the simplest second-order derivative (assuming that vertical grid spacing is constant) would be
kappa_FL*(uw(i1,k-1,iCell) - 2.0_RKIND*uw(i1,k,iCell) + uw(i1,k+1,iCell)) / ( 0.5_RKIND*(ze(k-1,iCell) - ze(k+1,iCell))**2.0_RKIND)The coefficients for the buoyancy pressure closure change between the different budgets (w'w' contains
C2while all the other budgets containbeta5). Are these connected in your parameter definitions (C2=1-beta5for energy conservation?), and if so could they be combined for simplicity in the code? It also looks likeBcould be used to replace the buoyancy flux in the w'w' budget as in the other budgets.MPAS-Model/src/core_ocean/shared/mpas_ocn_adcReconstruct.F
Lines 512 to 513 in 4923b0e
MPAS-Model/src/core_ocean/shared/mpas_ocn_adcReconstruct.F
Line 605 in 4923b0e