The equation of time describes the discrepancy between two kinds of solar time. The word equation is used in the medieval sense of reconcile a difference. The two times that differ are the apparent solar time, which directly tracks the motion of the sun, and mean solar time, which tracks a theoretical "mean" sun with noons 24 hours apart.
(from Wikipedia)
In the Mathematica documentation for SiderealTime, there is an "application" sample to "plot the equation of time by finding the difference between the Sun's right ascension at noon and the sidereal time at noon":
sunpos = SunPosition[GeoPosition[{0, 0}],
DateRange[DateObject[{2014, 1, 1, 12, 0}, TimeZone -> 0],
DateObject[{2014, 12, 31, 12, 0}, TimeZone -> 0], 10],
CelestialSystem -> "Equatorial"];
stime = SiderealTime[GeoPosition[{0, 0}],
DateRange[DateObject[{2014, 1, 1, 12, 0}, TimeZone -> 0],
DateObject[{2014, 12, 31, 12, 0}, TimeZone -> 0], 10]];
equationoftime =
TimeSeriesThread[With[{diff = First[#][[1]] - Last[#]},
UnitConvert[
Mod[diff, Quantity[24, "HoursOfRightAscension"],
Quantity[-12, "HoursOfRightAscension"]],
"MinutesOfRightAscension"]] &, {sunpos, stime}];
DateListPlot[equationoftime, FrameLabel -> Automatic]

As you can see, the "amplitude" of the plot is different from the "amplitude" of the plot on Wikipedia. On may sources, graphical or tabular, the first maximum is less than $15^m$ and the last minimum is deeper than $-15^m$.
So, my questions (if someone knows):
- What is the reason for these differences
- What effects are taken into account by these astronomical functions? (nutation?) For example does
SiderealTimereturn the LAST or the mean ST? - What are the bibliographic sources and the formula used by these astronomical functions?
