Equation of time
The equation of time is essentially the addition of a sundial to the modern wristwatch. It measures time according to the current position of the sun, by which the length of a day can vary by -16 to +14 minutes compared to average or civil time. The difference is called the equation of time. For practical reasons, man has divided each year into 365 and a quarter days, each day into 24 hours, and the hours into 60 minutes each. However, because the Earth’s orbit is elliptical rather than circular, the time in relation to the sun varies daily. It is exactly 24 hours long on only four days: April 15th, June 14th, September 1st and December 24th.