Conversion between vapor pressure (e), vapor pressure deficit (VPD), specific humidity (q), and relative humidity (rH).
VPD.to.rH(VPD, Tair, Esat.formula = c("Sonntag_1990", "Alduchov_1996",
"Allen_1998"), constants = bigleaf.constants())rH.to.VPD(rH, Tair, Esat.formula = c("Sonntag_1990", "Alduchov_1996",
"Allen_1998"), constants = bigleaf.constants())
e.to.rH(e, Tair, Esat.formula = c("Sonntag_1990", "Alduchov_1996",
"Allen_1998"), constants = bigleaf.constants())
VPD.to.e(VPD, Tair, Esat.formula = c("Sonntag_1990", "Alduchov_1996",
"Allen_1998"), constants = bigleaf.constants())
e.to.VPD(e, Tair, Esat.formula = c("Sonntag_1990", "Alduchov_1996",
"Allen_1998"), constants = bigleaf.constants())
e.to.q(e, pressure, constants = bigleaf.constants())
q.to.e(q, pressure, constants = bigleaf.constants())
q.to.VPD(q, Tair, pressure, Esat.formula = c("Sonntag_1990",
"Alduchov_1996", "Allen_1998"), constants = bigleaf.constants())
VPD.to.q(VPD, Tair, pressure, Esat.formula = c("Sonntag_1990",
"Alduchov_1996", "Allen_1998"), constants = bigleaf.constants())
Vapor pressure deficit (kPa)
Air temperature (deg C)
Optional: formula to be used for the calculation of esat and the slope of esat.
One of "Sonntag_1990"
(Default), "Alduchov_1996"
, or "Allen_1998"
.
See Esat.slope
.
eps - ratio of the molecular weight of water vapor to dry air (-) Pa2kPa - conversion pascal (Pa) to kilopascal (kPa)
Relative humidity (-)
Vapor pressure (kPa)
Atmospheric pressure (kPa)
Specific humidity (kg kg-1)
Foken, T, 2008: Micrometeorology. Springer, Berlin, Germany.