Please forgive me if this is a dumb question, or if my understanding of basic physics is wrong. Please feel free to correct me.
As I understand it, if the Earth didn't have any atmosphere, then the time of sunrise would be the point when the Sun's rays approached your position at a tangent. For example, imagine that the Earth is a perfect sphere, with you standing on top, and the (apparent) motion of the Sun was it travelling clockwise as follows (scales completely wrong, but hopefully the concept is correct)...
Now, assume for simplicity that the Earth's atmosphere is of constant destiny, and starts at a defined height above the planet's surface, then (if I understand correctly), the Sun's rays would be refracted as they entered the atmosphere, meaning that you would see the sun slightly earlier (exaggerated)...
Obviously, this is very simplified, not least because the atmosphere is a gas, and therefore of variable density, presumably being less dense the higher you went. I imagine that the variation in density would mean that the rays appeared to curve, rather than take a sudden turn as shown above.
My question is, how much difference does the air temperature make to the amount of diffraction, which in turn affects the time at which you would see the sunrise? My feeling is that if it were cold across the Earth, then the air would be more dense, resulting in a greater degree of refraction, and so an earlier sunrise. By contrast, a higher temperature would mean lower density, less refraction and a later sunrise.
Anyone able to give me some estimates of how much difference you would expect to see between a warm summer's day and a cold winter's day, assuming normal parameters for "cold" and "warm" for our planet?