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An estimate of mean pressure at a given elevation as predicted by the hypsometric equation.
pressure.from.elevation( elev, Tair, VPD = NULL, constants = bigleaf.constants() )
Atmospheric pressure (kPa)
Elevation a.s.l. (m)
Air temperature (deg C)
Vapor pressure deficit (kPa); optional
Kelvin- conversion degC to Kelvin pressure0 - reference atmospheric pressure at sea level (Pa) Rd - gas constant of dry air (J kg-1 K-1) g - gravitational acceleration (m s-2) Pa2kPa - conversion pascal (Pa) to kilopascal (kPa)
Atmospheric pressure is approximated by the hypsometric equation:
$$pressure = pressure_0 / (exp(g * elevation / (Rd Temp)))$$
Stull B., 1988: An Introduction to Boundary Layer Meteorology. Kluwer Academic Publishers, Dordrecht, Netherlands.
# mean pressure at 500m altitude at 25 deg C and VPD of 1 kPa pressure.from.elevation(500,Tair=25,VPD=1)
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