View source: R/evapotranspiration.r
reference.ET | R Documentation |
Reference evapotranspiration calculated from the Penman-Monteith equation with a prescribed surface conductance. This function is deprecated. Use potential.ET(...,approach="Penman-Monteith") instead.
reference.ET( data, Gs_ref = 0.0143, Tair = "Tair", pressure = "pressure", VPD = "VPD", Rn = "Rn", Ga = "Ga_h", G = NULL, S = NULL, missing.G.as.NA = FALSE, missing.S.as.NA = FALSE, Esat.formula = c("Sonntag_1990", "Alduchov_1996", "Allen_1998"), constants = bigleaf.constants() )
data |
Data.frame or matrix containing all required variables; optional |
Gs_ref |
Reference surface conductance (m s-1); defaults to 0.0143 m s-1. |
Tair |
Air temperature (degC) |
pressure |
Atmospheric pressure (kPa) |
VPD |
Vapor pressure deficit (kPa) |
Rn |
Net radiation (W m-2) |
Ga |
Aerodynamic conductance to heat/water vapor (m s-1) |
G |
Ground heat flux (W m-2); optional |
S |
Sum of all storage fluxes (W m-2); optional |
missing.G.as.NA |
if |
missing.S.as.NA |
if |
Esat.formula |
Optional: formula to be used for the calculation of esat and the slope of esat.
One of |
constants |
cp - specific heat of air for constant pressure (J K-1 kg-1) |
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