The earth rotates uniformly once per 24 hours in this frame (mean solar
time). Let a point on the earth's surface P define a unit vector
at the origin of the frame. The azimuth angle
of this vector is
measured as usual in the X-Y plane from the X-axis, so in a day,
covers the complete range of 0 to 360 degrees. Generally, time zones
are chosen so that at some longitude in the zone,
at noon. To simplify, let P have this longitude, at latitude
.
Then
is a measure of time of day at P with respect to noon. If we can
find where vector
is at sunrise, then that value of
will give us the time of sunrise.
The explicit relationship between the vector xyz components and angles
and
is
If P were in a different place in the time zone, i.e. P had a different longitude from that assumed above, a constant shift would occur in the times of sunrise, sunset, and sun's highest elevation.
We will take the latitude of the observer to be
.