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Saturation vapor pressure calculation does not change at negative temperatures #592

@bsu-wrudisill

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@bsu-wrudisill

Hello,

I would like to raise a question — it appears that the saturation vapor pressure of ice and liquid water are treated the same in summa.
There's only a formula for the saturation vapor pressure with respect to water in the conv_funcs.f90 file:

subroutine satVapPress(TC, SVP, dSVP_dT)

And, in the vegNrgFlux code, the saturation vapor pressure of the ground is computed this way:

call satVapPress(TG_celcius, scalarSatVP_GroundTemp, dSVPGround_dGroundTemp)

TG_celcius = groundTemp - Tfreeze
call satVapPress(TG_celcius, scalarSatVP_GroundTemp, dSVPGround_dGroundTemp)

So, I don't think that the saturation vapor pressure with respect to ice is ever used for the snow surface? I think that TG_celcius is just the snow temperature of the uppermost layer in this case (if there is snow on the ground).

I actually care about the atmospheric water deposition process (which happens at cold temperatures) so I think that this might be an important process that depends quite strongly on how the surface vapor pressure is calculated!

Thank you. Please let me know if I'm mistaken about this.

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