00:01
Here we say we have a light ray entering the atmosphere.
00:06
We'll have that be the edge of our atmosphere, where it descends vertically to the surface.
00:12
I guess it's fine.
00:15
This is the surface of the earth.
00:19
So the index of a fraction right here is given at n equals 1.
00:25
And then when it gets to the surface, we get a index of just n.
00:30
They say it is a linear progression, so it's linearly changing from one to whatever n is.
00:40
And so the first question they ask is, how long does it take the ray to traverse this path? so like what's the time it takes to get from there to there? and so what we can do is we can take, because it's linear, we can take the average of these two, which is just n plus 1 over 2 is going to be our n.
01:03
An average, which we can use because it's linear for that index during that time.
01:08
And again, the index is just how much it's slowing down compared to the speed of light.
01:15
So let's just say the actual speed, right, divided by the speed of light, is that n.
01:21
So n plus 1 over 2.
01:23
And so the speed of that light is just the speed of light times n plus 1...