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seasalt.f90 (does not cite anything, powerlaw relationship similar to Sutherland's law)
L758-775
visc0air = 1.75e-5_r8, & !// Viscosity of air at temperature T0visc
T0visc = TK_0C, & !// Temperature at which visocity=visc0 (K)
nviscair = 0.65_r8 !// Power law dependence viscosity on T
!// Viscocity of air at ambient temperature
viscair = visc0air * (TEM(L) / T0visc)**nviscair
Later on in the same code we have it duplicated (L908-940)
!// VISCOCITY OF AIR
viscair = visc0air * (TEM / T0visc)**nviscair
drydeposition_oslo.f90 (citing Prather, PBL using some wired linear fit through origin to describe the powerlaw relation, states "abs.visc.")
L1489-1492
Update:
I have tested the range of z0 and the resulting Rb for both parametrizations of the dynamic viscosity. Well, I only ran the model for one entire day, though.
The good news first: The difference in Rb is only about 1.4%. Meaning the average Rb using the "Prather"-fit is only about 1.4% smaller than it would have been using Sutherland's law.
This is mainly due to the fact that Rb is generally, in about 91% (88%) of all cases, below the threshold of 10 sm^-1 (see dynamic_viscosity_diffs.pdf dynamic_viscosity_zo_Rb.pdf).
Calculating the weighted mean for both Rb distributions, while setting all values which appear below the threshold to the threshold value:
Recently, I have found at least three different definitions of "dynamic viscosity" throughout different parts of the model:
L560
L758-775
Later on in the same code we have it duplicated (L908-940)
L1489-1492
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