R_a: Radiation, extraterrestrial solar

Description Usage Arguments Value References

View source: R/radiation_functions.R

Description

Calculates the extraterrestrial radiation for a given location and timestep. For daily periods, uses Equation 21 from Allen et al. (1998). For hourly or shorter periods, uses Equation 28 from Allen et al. (1998).

Usage

1
R_a(dt, datetimes, phi, Lm, Lz, Gsc = 0.082)

Arguments

dt

a string indicating the timestep of calculation. If not "hourly", assumes a daily or larger timestep

datetimes

timeseries of datetimes to use in calculations POSIXct

phi

latitude of the location (radians). Positive for northern hemisphere, negative for southern hemisphere.

Lm

longitude of the measurement site (degrees west of Greenwich).

Lz

longitude of the center of the time zone used for measurements (degrees west of Greenwich). For example, Lz = 75, 90, 105 and 120° for the Eastern, Central, Rocky Mountain and Pacific time zones (United States) and Lz = 0° for Greenwich, 330° for Cairo (Egypt), and 255° for Bangkok (Thailand).

Gsc

solar constant (MJ/m^2/min). Defaults to 0.0820 MJ/m^2/min.

Value

Ra

extraterrestrial radiation (MJ/m^2/day) or (MJ/m^2/hour), depending on length of input time period

References

Allen, R. G., Pereira, L. S., Raes, D., & Smith, M. (1998). Crop evapotranspiration: Guidelines for computing crop water requirements. Rome: FAO. Retrieved from http://www.fao.org/docrep/X0490E/x0490e00.htm.


WDNR-Water-Use/CSLSevap documentation built on April 9, 2021, 1:35 a.m.