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sidereal time and time scales

    Sidereal Time is based on the Earth's sidereal rotation period (rotation with respect to the stars). The length of the sidereal day is 24 sidereal hours, or 23h56m4s Solar time. The difference is due to the angular motion of the earth around the Sun. In a year there is one more sidereal day than Solar day. The sidereal time is a measured locally. The local sideral time (LST) is the right ascension of the zenith. The hour angle HA of an object with right ascension RA is given by HA=LST-RA GMST (Greenwich Mean Sidereal Time) at 0h UT = 24110.54841 + 8640184.812866 TU + 0.093104TU^2 - 6.2x10-6TUT^3 seconds GAST (Greenwich Apparent Sidereal Time) = GMST + the equation of the equinoxes. The Equation of the Equinoxes is the total nutation in longitude time the cosine of the true obliquity of the ecliptic. It ranges from +0.8 to +1.2 seconds. LAST (Local Apparent Sidereal Time) is the hour angle of the ascending node of the ecliptic. LMST (Local Mean Sidereal Time) = GMST - geode...