The sidereal day is defined to be the length of time for the vernal equinox to return to your celestial meridian. The solar day is defined to be the length of time for the Sun to return to your celestial meridian. The two are not the same, as illustrated in the following animation.
Because the Earth is in motion on its orbit around the Sun in the course of a day, the Earth must turn about four minutes longer each day (3 minutes and 56 seconds, to be exact) to bring the Sun back to the celestial meridian than to bring the vernal equinox back to the celestial meridian. Thus, the solar day is 3 minutes and 56 seconds longer than the sidereal day. (In this animation the angle corresponding to four minutes of rotation has been exaggerated for clarity.) The difference between the length of the solar and sidereal days for Earth is not very large because the period for the Earth to rotate on its axis is small compared with the period for one revolution around the Sun. For some other planets the difference is much larger, as described in the box below. For example, the length of the solar day on Mercury is two sidereal (Mercury) years.
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