The length of the day was calculated by doubling the equation for the Hour Angle H between a transit of the sun and sunset:
H (of sunset) = arccos ( - tan(a)*tan(delta) ) .
The length of the day was calculated by doubling the equation for the Hour Angle H between a transit of the sun and the apparent sunset (or sunrise):
H (of sunset) = arccos (( cos (z) - sin(a)*sin(delta)) / (cos(a)*cos(delta)) ) .
CITY | LATITUDE (N) | LONGITUDE (E) | London | 51 | 0 | Tel Aviv | 32 | 35 |
Cairo | 30 | 31 |
Wien | 48 | 16 |
New York | 41 | -74 (74W) |
Tokyo | 35 | 140 |
Singapore | 1 | 104 |
Manila | 14 | 121 |
Bangkok | 13 | 100 |
Anchorage (ALASKA) | 61.2 | -150 |
Tucson | 32.25 | -110.95 |
Addis Ababa | 9 | 39 |
Phoenix | 33.5 | -112.05 |
Prepared by A.C. from the