Coordinate Systems

Let us define the coordinate system used for most astronomical observations. To define positions of objects on the Celestial Sphere, we use a system analogous to longitude and latitude. So now let's begin. Because the spin axis of the Earth and the orbital axis of the Earth are not parallel (they form an angle = 23.5 degrees), the Ecliptic and the Celestial Equator are inclined with respect to each other. This gives us some natural checkpoints on the sky (spheres have no ears to grab). We define the following points on the Celestial Sphere;

Vernal (Mar 21) and Autumnal (Sep 21) Equinoxes and Winter (Dec 21) and Summer (June 21) Solstices

The two equinoxes occur when the Sun passes through the Celestial Equator and the two solstices occur when the Sun is at its greatest distance above and below the Celestial Equator.

We define:

So, for example,