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.frame or matrix containing all required variables; optional
Reference surface conductance (m s-1); defaults to 0.0143 m s-1.
Air temperature (degC)
Atmospheric pressure (kPa)
Vapor pressure deficit (kPa)
Net radiation (W m-2)
Aerodynamic conductance to heat/water vapor (m s-1)
Ground heat flux (W m-2); optional
Sum of all storage fluxes (W m-2); optional
if TRUE
, missing G are treated as NA
s, otherwise set to 0.
if TRUE
, missing S are treated as NA
s, otherwise set to 0.
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
.
cp - specific heat of air for constant pressure (J K-1 kg-1)
eps - ratio of the molecular weight of water vapor to dry air
Rd - gas constant of dry air (J kg-1 K-1) (only if approach = "Penman-Monteith"
)
Rgas - universal gas constant (J mol-1 K-1) (only if approach = "Penman-Monteith"
)
Kelvin - conversion degree Celsius to Kelvin (only if approach = "Penman-Monteith"
)