I’ve been poking around Wikipedia this morning and found this pearl of wisdom, if I might paraphrase here a bit … when a physicist attempts to explain something, they like to use the simplest explanation … and for some phenomena this simplest explanation uses a rotating frame-of-reference and the Coriolis force that appears in this frame … it’s not that these phenomena can’t be explained in a stationary frame-of-reference … but it gets very complicated fairly quickly …
For example … if we wish to explain the motion of the Moon around the Sun … it’s easiest to invoke the pseudo-force of gravity … the “action from a distance” explains how the Moon orbits the Earth and how the Earth orbits the Sun … compare that to using the intersection of two surfaces of revolution in time/space … 99.9% of your audience will be lost as soon as we mention “field tensor” … and in this case the differences are so minute that Newton’s Law of Gravity is close enough …
Are pseudo-forces “real”, who knows … are they useful, you bet …
I think this really cool educational film from 1960, courtesy of the University of Toronto, might help understanding the things related to frames of reference in physics. Link follows:
Consider a rock swinging around on a rope of length L, with rotational frequency of w radians per second.
While the rock is still tethered to the rope, the x coordinate will be Lcos(wt) and the y coordinate will be Lsin(wt) at all times. In coordinates rotating with the rock, r=L and theta is 0 for all times (the rotating frame has theta=wt relative to the non-rotating frame).
For convenience, we’ll cut the rope at time 0 when the rock is at x=L and y=0, moving in the y direction at a speed of wL.
After that time, x remains L for all time, and y=wLt.
What does this look like in the rotating frame?
Rnew=square root (L^2+w^2L^2t^2) and thetanew=arc tan (w*t)-wt
As long as the small angle approximation applies, Rnew is approximately L+L*(1+w^2L^2t^2/2) and thetanew = wt- (wt)^3/3 - and for very short times that means that it looks like the rock is moving away from where it was at an acceleration of w^2*L^2/2