
So the epicycles were the result of using ω0 as the reference frequency which resulted in a steady increase of phase φ = ½Δωt.
In general one can simplify the above result a little more.

There is a steady tone at the reference frequency ω0 and one at the average of the two frequencies ϖ which is the one that fluctuates in amplitude. When a and b are equal the steady tone is not present and one just hears the warbling tone. The second term shifts in phase and amplitude relative to the first. That's the "epicycle".
Try listening to the shorter intervals such as the tone or semitone in the Wikipedia particular number article. There's a bit of a quaver present. One could also try simultaneously playing two neighboring keys on a piano or notes on a guitar.
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