- #36
russ_watters
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It just so happens someone posted a discussion of exactly what I'm referring to in another thread (the second diagram shows it):russ_watters said:Hurkyl, what I think I'm seeing for the near side doesn't sound like any of those:
The tidal force creates a near-side bulge and flattens the far side.
Then #4 would explain the far side bulge.
http://www.lhup.edu/~dsimanek/scenario/tides.htmOne of the few books that clearly defines "tide" at the outset is The Planetary System by Morrison and Owen [1966]: "A tide is a distortion in the shape of one body induced by the gravitational pull of another nearby object." This is definition (2) above. It clearly says that tides are the result of gravitation, without any mention of rotation effects...
Now here's where it gets really interesting:
That's a twist I actually wasn't aware of, but of course it makes sense: The barycenter is not a fixed point that the Earth rotates around, but a virtual point that moves as the moon moves around the earth.In this representation [the centrifugal force misconception] we can treat this system as if it were an inertial system, but only at the expense of introducing the concept of centrifugal force. It turns out that when this is done, the centrifugal force on a mass anywhere on or within the Earth is of constant size, and is therefore equal to the size of the gravitational force the moon exerts on the same amount of mass at the center of the Earth... ...
We are now focusing on the effects due only to the Earth-moon system. The motion of the Earth about the Earth-moon center of mass, causes every point on or within the Earth to move in an arc of the same radius. This is a geometric result most books totally ignore, or fail to illustrate properly. Therefore every point on or within the Earth experiences the same size centrifugal force. A force of constant size throughout a volume cannot give rise to tidal forces (as we explained above). The size of the centrifugal force is the same as the force the moon exerts at the Earth-moon center of mass (the barycenter), where these two forces are in equilibrium. [This barycenter is 3000 miles from the Earth center—within the Earth's volume.]