The fundamental unit of solar time is the day, based on the synodic rotation period.
[1] A tall pole vertically fixed in the ground casts a shadow on any sunny day.
At one moment during the day, the shadow will point exactly north or south (or disappear when and if the Sun moves directly overhead).
[2] This is "mean solar time", which is still not perfectly constant from one century to the next but is close enough for most purposes.
It is based on the apparent solar day, the interval between two successive returns of the Sun to the local meridian.
[b] The length of a solar day varies through the year, and the accumulated effect produces seasonal deviations of up to 16 minutes from the mean.
Therefore, apparent solar days are shorter in March and September than in June or December.
The sun has always been visible in the sky, and its position forms the basis of apparent solar time, the timekeeping method used in antiquity.
[19] It is not clear if they knew of the variation in the length of the solar day and the corresponding equation of time.
[20] Apparent solar time grew less useful as commerce increased and mechanical clocks improved.