The period between two successive transits of a particular meridian on the earth by the apparent sun. Because of the elliptical shape of the earth's orbit, the apparent angular velocity of the sun as seen is not constant, or the apparent sun's (also called
true sun velocity is not constant; hence, the days as indicated by the apparent travel of the true or apparent sun are not of uniform length. To make solar days of uniform length, astronomers have invented the mean sun, a fictitious body imagined to move at a uniform rate along the celestial equator, thus making a complete circuit from west to east in one year.