For the following, I’m thinking of Europa as a point of mass, which is obviously wrong as far as tides go (and probably not what DrMatrix is thinking of), but this will make my thoughts more clear (I hope.) I’m repeating a lot of what g8rguy is saying, but maybe in a slightly different way.
For a point mass in the inertial frame you can’t have an acceleration due to rotation. The rotation/revolution of the moon is due to acceleration–the acceleration of gravity. The rotation cannot cause another acceleration. (I realize this isn’t what you were saying, Doc, but this is why I was balking.)
Indeed–for a rigid rotating disk, where the force accelerating the points on the disk is the mechanical strength of the disk itself, you’re right. However, in an orbital system, the acceleration is indeed 1/r[sup]2[/sup]. You can’t get an infinite acceleration because eventually you’d be inside the planet and the mass above you wouldn’t be contributing to the gravitational force. (This all breaks down for a black hole, which are infinitely dense–the acceleration does go to infinity at r=0.)
Maybe the two points of view could be reconciled by remembering that Europa is, of course, not a point mass, and all points on Europa are not orbiting the planet independently; the center of mass of Europa is orbiting the planet, and all the mass of Europa is forced to follow the same path as the center of mass; thus all points have the same angular velocity, w, across Europa the centripetal acceleration is proportional to the distance from Jupiter.
This may have been what DrMatix was trying to say all along.
In review, the acceleration of the center of mass of Europa is proportional to 1/r[sup]2[/sup]. The whole body is accelerated in this way, producing the angular velocity, w. Now, ignoring Jupiter’s gravity, considering only Europa’s motion, the force a point in Europa feels is depends linearly on its distance from Jupiter.
For the center of mass, a=GM/R[sup]2[/sup]=w[sup]2[/sup]R where R is the distance from Jupiter to the center of mass, leading to w[sup]2[/sup]=GM/R[sup]3[/sup]. Then for any other point on Europa, at a distance r from Jupiter, so the accleration DrMatix was talking about is a=GMr/R[sup]3[/sup]. Right?
How does this help us understand tides? There’s an acceleration, pointing in the same direction as gravity, but a bit stronger.
But luckily, this is irrelevant; Europa isn’t a rigid body; it’s a fluid body–otherwise there’d be no tides. To some degree, each point on Europa is orbiting on its own, but is constrained by Europa’s self-gravity (not predominatly by mechanical strength). The points are not accelerated as a=GMr/R[sup]3[/sup]; they accelerate as a=GM/r[sup]2[/sup](in Jupiter’s direction)-Gm/p[sup]2[/sup] (toward Europa’s center), where m is Europa’s mass and p is the distance from the point to Europa’s center of mass.
Think of Europa as (almost) a sphere. Then the pull toward Europa’s center is the same for all points at the surface, while the acceleration of Jupiter’s gravity is much stronger at the front than the back. Thus the front falls toward Jupiter faster, and the back falls more slowly, and Europa stretches.
My head hurts and I am hungry. There may be errors above, and I hope you will point them out.