This function returns the solar angles at a given time and location.
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sun_angles( time = lubridate::now(tzone = "UTC"), tz = lubridate::tz(time), geocode = tibble::tibble(lon = 0, lat = 51.5, address = "Greenwich"), use.refraction = FALSE ) sun_angles_fast(time, tz, geocode, use.refraction) sun_elevation( time = lubridate::now(), tz = lubridate::tz(time), geocode = tibble::tibble(lon = 0, lat = 51.5, address = "Greenwich"), use.refraction = FALSE ) sun_zenith_angle( time = lubridate::now(), tz = lubridate::tz(time), geocode = tibble::tibble(lon = 0, lat = 51.5, address = "Greenwich"), use.refraction = FALSE ) sun_azimuth( time = lubridate::now(), tz = lubridate::tz(time), geocode = tibble::tibble(lon = 0, lat = 51.5, address = "Greenwich"), use.refraction = FALSE )
A "vector" of POSIXct Time, with any valid time zone (TZ) is allowed, default is current time.
character string indicating time zone to be used in output.
data frame with variables lon and lat as numeric values (degrees), nrow > 1, allowed.
logical Flag indicating whether to correct for fraction in the atmosphere.
This function is an implementation of Meeus equations as used in NOAAs on-line web calculator, which are precise and valid for a very broad range of dates (years -1000 to 3000 at least). The apparent solar elevations near sunrise and sunset are affected by refraction in the atmosphere, which does in turn depend on weather conditions. The effect of refraction on the apparent position of the sun is only an estimate based on "typical" conditions for the atmosphere. The computation is not defined for latitudes 90 and -90 degrees, i.e. exactly at the poles.
In the current implementation functions
sun_zenith_angle are wrappers
sun_angles, so if more than one angle is needed it is
preferable to directly call
sun_angles as it will be faster.
A data.frame with variables time (in same TZ as input), TZ, solartime,
longitude, latitude, address, azimuth, and elevation. If a data frame with
multiple rows is passed to
geocode and a vector of times longer
than one is passed to
time, sun position for all combinations of
locations and times are returned are returned by
contrast, convenience functions returning a vector.
There exists a different R implementation of the same algorithms called
"AstroCalcPureR" available as function
astrocalc4r in package
'fishmethods'. Although the equations used are almost all the same, the
function signatures and which values are returned differ. In particular,
the present implementation splits the calculation into two separate
functions, one returning angles at given instants in time, and a
separate one returning the timing of events for given dates.
The primary source for the algorithm used is the book: Meeus, J. (1998) Astronomical Algorithms, 2 ed., Willmann-Bell, Richmond, VA, USA. ISBN 978-0943396613.
A different implementation is available at https://apps-nefsc.fisheries.noaa.gov/AstroCalc4R/ and in R paclage 'fishmethods'. In 'fishmethods' (= 1.11-0) there is a bug in function astrocalc4r() that affects sunrise and sunset times.
An interactive web page using the same algorithms is available at https://www.esrl.noaa.gov/gmd/grad/solcalc/. There are small differences in the returned times compared to our function that seem to be related to the estimation of atmospheric refraction (about 0.1 degrees).
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