The equation of time
This is the equation for the difference between
mean and apparent solar time.
Solar time gives days that are not of continuous length. The length of a
solar day varies due to:
(a) the fact that the Earth goes round the Sun in an ellipse and
so moves at different speeds at different times of the year
(b) the Earth's axis is inclined
at 23.5
o to the plane of the orbit
| Date |
Minutes |
|
Date |
Minutes |
| January 1 |
-3.2 |
|
July 1 |
-3.5 |
| January 16 |
-9.6 |
|
July 16 |
-5.9 |
| February 1 |
-13.5 |
|
August 1 |
-6.3 |
| February 16 |
-14.2 |
|
August 16 |
-4.4 |
| March 1 |
-12.6 |
|
September 1 |
-0.2 |
| March 16 |
-9.0 |
|
September 16 |
+4.8 |
| April 1 |
-4.2 |
|
October 1 |
+10.0 |
| April 16 |
-0.0 |
|
October 16 |
+14.2 |
| May 1 |
+2.8 |
|
November 1 |
+16.3 |
| May 16 |
+3.7 |
|
November 16 |
+15.3 |
| June 1 |
+2.4 |
|
December 1 |
+11.3 |
| June 16 |
-0.4 |
|
December 16 |
+4.8 |
A VERSION IN WORD IS AVAILABLE ON THE SCHOOLPHYSICS USB