This block computes the wet bulb temperature for a given dry bulb temperature, relative air humidity and atmospheric pressure.
If the constant approximateWetBulb
is true
,
then the block uses the approximation of Stull (2011) to compute
the wet bulb temperature without requiring a nonlinear equation.
Otherwise, the model will introduce one nonlinear equation.
The approximation by Stull is valid for a relative humidity of 5% to 99%,
a temperature range from -20°C to 50°C
and standard sea level pressure.
For this range of data, the approximation error is -1 Kelvin to +0.65 Kelvin,
with a mean error of less than 0.3 Kelvin.
Otherwise a calculation based on an energy balance is used. See #474 for a discussion. The model is validated in IBPSA.Utilities.Psychrometrics.Examples.TWetBul_TDryBulPhi.
For a model that takes the mass fraction instead of the relative humidity as an input, see IBPSA.Utilities.Psychrometrics.TWetBul_TDryBulXi.
Stull, Roland. Wet-Bulb Temperature from Relative Humidity and Air Temperature Roland Stull. Journal of Applied Meteorology and Climatology. Volume 50, Issue 11, pp. 2267-2269. November 2011 DOI: 10.1175/JAMC-D-11-0143.1
Name | Description |
---|---|
Medium | Medium model |
IBPSA.Utilities.Psychrometrics.Functions.saturationPressure()
and
IBPSA.Utilities.Psychrometrics.Functions.saturationPressureLiquid()
as these functions have been moved from the medium to the psychrometrics package.