ETref | R Documentation |
FAO Penman-Monteith equations to compute grass reference evapotranspiration from weather data for daily, monthly, hourly or shorter periods.
ETref( x, Tmax = NULL, Tmin = NULL, Rhmax = NULL, Rhmin = NULL, Tmean = NULL, Rhmean = NULL, u = NULL, Rs = NULL, n = NULL, P = NULL, elev, lat.rad = NULL, lat.deg = NULL, long.deg = NULL, tl, G = NULL, actVP = NULL, control = list() )
x |
date-time object or day of the year (must be date-time object if calculation period is shorter than a day) |
Tmax |
maximum temperature [degreeC] during 24-hour period (for daily values) |
Tmin |
minimum temperature [degreeC] during 24-hour period (for daily values) |
Rhmax |
maximum of air humidity [percent] during 24-hour period (for daily values) |
Rhmin |
minimum of air humidity [percent] during 24-hour period(for daily values) |
Tmean |
mean air temperature [degreeC]. For periods shorter 1 day. |
Rhmean |
mean relative air humidity [percent]. For periods shorter 1 day or if Rhmax and Rhmin are missing. |
u |
wind speed [m/s] at 2 meter height. If measurement height is not 2 m, define height with control <- list(uz = 2) |
Rs |
solar radiation [MJ/(m2 time)] |
n |
actual hours of sunshine. Used to calculate Rs if Rs messurements are not available (see |
P |
air pressure [kPa]. Estimated with |
elev |
station elevation above sea level [m] |
lat.rad |
latitude [rad]. Use either lat.rad or lat.deg. Latitude is positive for the northern hemisphere and negative for the southern hemisphere |
lat.deg |
latitude [degree]. Use either lat.deg or lat.rad. Latitude is positive for the northern hemisphere and negative for the southern hemisphere |
long.deg |
longitude [degree] east of Greenwich (for periods < 1 day) |
tl |
length of calculation period [hour] (1 for hourly, 0.5 for 30-minute and 24 for daily period). Only needed if x is date-time object with length of 1. |
G |
soil heat flux (Assumed to be 0 for daily calculations) (for calculation periods shorter than a day estimated with |
actVP |
Actual vapor pressure [kPa]. If Rhmax, Rhmin and Rhmean are NULL |
control |
list for control parameters and empirical factors (see details, |
must be provided as.numeric (1-366) or as a common date-time object (e.g, POSIXct, POSIXlt or Date objects). All formats for which is.timepoint from the lubridate package returns TRUE can be used
controlDefaults
and constDefaults
)Lz:
longitude of the centre of the local time zone (degrees west of Greenwich)
- 0 for Greenwich
- 345 for Germany
- 330 for Cairo (Egypt)
- 255 for Bangkok (Thailand)
- 75, 90, 105 and 120 for Eastern, Central, Rocky Mountain and Pacific time zones (United States)
Lz is only needed if calculation period is shorter than 1 day.
uz: height of wind measurements (m)
albedo: default 0.23 for the hypothetical grass and alfalfa reference crops used in
the FAO-56 PM equations
as: regression constant, expressing fraction of extraterrestrial radiation reaching earth on overcast days (n = 0) (default = 0.25)
bs: as + bs fraction of extraterrestrial radiation reaching earth on clear days (n = N) (default = 0.5)
Tko: reference temperature [degreeC] at elevation z0. Only needed if atmospheric pressure is missing. Often assumed to be 20 degreeC.
z0: elevation at reference level (fefault = 0 [m])
est.ratio.Rs.Rso:
Rs/Rso is used to represent cloud cover. For hourly or shorter periods during the nighttime,
the ratio Rs/Rso is set equal to the Rs/Rso calculated for a time period occurring 2-3 hours before sunset.
If single values during nighttime are calculated Rs/Rso ration 2-3 hours before sunset can not be calculated
and an approximation is needed. Following Allen (1999) one can assume Rs/Rso = 0.4 to 0.6 during nighttime periods
in humid and subhumid climates and Rs/Rso = 0.7 to 0.8 in arid and semiarid climates. A value of Rs/Rso = 0.3 presumes
total cloud cover.
grass reference evapotranspiration [mm]
eq. 6 from reference for daily and eq. 53 for hourly or shorter periods
Ullrich Dettmann
Allen, R. G., Pereira, L. S., Raes, D., & Smith, M. (1998). Crop evapotranspiration-Guidelines for computing crop water requirements-FAO Irrigation and drainage paper 56. FAO, Rome, 300(9).
# -------------------------------------------- # Daily Evapotranspiration # -------------------------------------------- ETref(x = 187, Rs = 22.07, elev = 100, lat.deg = 50.8, Tmax = 21.5, Tmin = 12.3, Rhmax = 84, Rhmin = 63, u = 2.78, control = list(uz = 10), P = 100.1) # Calculation with sunshine hour (n) instead of # global radiation (Rs) (Rs ist estimated from n with estRs): ETref(x = 187, n = 9.25, elev = 100, lat.deg = 50.8, Tmax = 21.5, Tmin = 12.3, Rhmax = 84, Rhmin = 63, u = 2.78, control = list(uz = 10), P = 100.1) # -------------------------------------------- # Hourly Evapotranspiration # -------------------------------------------- ETref(x = as.POSIXct(c('2018-10-01 14:30', '2018-10-01 15:30')), Tmean = c(38, 37.8), Rhmean = c(52, 52.3), u = c(3.3, 3.2), Rs = c(2.450, 2.5), elev = 8, lat.deg = 16.22, long.deg = 343.75, G = c(0.175, 0.178) , P = c(101.21, 101.21) , control = list(Lz = 15)) # If only one time step is calculated tl must be provided (1 for hourly, 0.5 for 30 minute periods): ETref(x = as.POSIXct('2018-10-01 14:30'), tl = 1, Tmean = 38, Rhmean = 52, u = 3.3, Rs = 2.450, elev = 8, lat.deg = 16.22, long.deg = 343.75, G = 0.1749218, P = 101.2056, control = list(Lz = 15)) # Calculation with missing soil heat flux (G) and atmospheric pressure (P) (G is estimated with estG # and P with estP) ETref(x = as.POSIXct('2018-10-01 14:30'), tl = 1, Tmean = 38, Rhmean = 52, u = 3.3, Rs = 2.450, elev = 8, lat.deg = 16.22, long.deg = 343.75, control = list(Lz = 15)) # --------------------------------------------
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