- Psychrometric constant
The psychrometric constant, , ralates the
partial pressure of water in air to the air temperature. This lets one interpolate actual vapor pressure from paired dry and wetthermometer bulb temperature readings [cite book |last=Allen |first=R.G. |coauthors=Pereira, L.S.; Raes, D.; Smith, M. |title=Crop Evapotranspiration—Guidelines for Computing Crop Water Requirements |url=http://www.fao.org/docrep/X0490E/x0490e00.HTM |accessdate=2007-10-08 |series=FAO Irrigation and drainage paper 56 |year=1998 |publisher=Food and Agriculture Organization of the United Nations |location=Rome, Italy |isbn=92-5-104219-5 ] .::
: psychrometric constant [kPa °C-1] ,
: P = atmospheric pressure [kPa] ,
:
latent heat of water vaporization, 2.45 [MJ kg-1] ,:
specific heat of air at constant pressure, [MJ kg-1 °C-1] ,: ratio
molecular weight of water vapor/dry air = 0.622.Both and are constants.
Sinceatmospheric pressure , P, depends upon altitude, so does .
At higheraltitude water evaporates and boils at lower temperature.Although is constant, varied air composition results in varied .
Thus on average, at a given location or altitude, the psychrometric constant is approximately constant. Still, it is worth remembering that weather impacts both atmospheric pressure and composition.
vapor pressure estimation
Saturated vapor pressure,
Actual vapor pressure,: here e [T] is vapor pressure as a function of temperature, T.::Tdew = the
dewpoint temperature at which water condenses.::Twet = the temperature of a wet thermometer bulb from which water can evaporate to air.::Tdry = the temperature of a dry thermometer bulb in air.References
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