Is there a reason why CLM4.5 used a squared formulation for the soil organic matter fraction (om_frac), and then CLM5 onwards uses an unsquared formulation? Is the squared formulation in CLM4.5 just a bug, or was there a particular reason for squaring om_frac in CLM4.5?
In the current CLM, there is a flag to use the old CLM4.5 formulation:
CTSM/src/biogeophys/SoilStateInitTimeConstMod.F90 at 7731d83c7fdb4bb31a3d0b5fc6eead3ea7ff4b29 · ESCOMP/CTSM
L56: logical, private :: organic_frac_squared ! If organic fraction should be squared (as in CLM4.5)
L480: om_frac = min(params_inst%om_frac_sf*organic3d(g,j+1)/organic_max, 1._r8)
L497: if (organic_frac_squared) then
om_frac = om_frac**2._r8
end if
The original paper, Lawrence and Slater 2008, Equation 1 uses an unsquared formulation, and CLM documentation also shows an unsquared formulation. But I can't find any papers/documentation/forums on how or why the CLM4.5 squared formulation originated.
Thanks for your help!
In the current CLM, there is a flag to use the old CLM4.5 formulation:
CTSM/src/biogeophys/SoilStateInitTimeConstMod.F90 at 7731d83c7fdb4bb31a3d0b5fc6eead3ea7ff4b29 · ESCOMP/CTSM
L56: logical, private :: organic_frac_squared ! If organic fraction should be squared (as in CLM4.5)
L480: om_frac = min(params_inst%om_frac_sf*organic3d(g,j+1)/organic_max, 1._r8)
L497: if (organic_frac_squared) then
om_frac = om_frac**2._r8
end if
The original paper, Lawrence and Slater 2008, Equation 1 uses an unsquared formulation, and CLM documentation also shows an unsquared formulation. But I can't find any papers/documentation/forums on how or why the CLM4.5 squared formulation originated.
Thanks for your help!