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I shouldn't presume to speak for David, but I don't think this accurately<http://www.intranet.csupomona.edu/%7Eajm>http://www.intranet.csupomona.edu/
reflects the important points he is trying to make.=A0 I *think* he is
saying (and I *know* I would contend) that there should be--**on
average**--two *measurable* tidal bulges of the *oceans* themselves which
are dragged ahead of the instantaneous Earth-Moon line and which are
important contributors to the angular momentum coupling in the Earth-Moon
system.=A0 These tidal bulges are raised in situ by the local gradient of
the Moon's gravitational field as it rushes around the Earth at whatever
"speed" it likes. They are almost entirely distinct from the "tides" that
are observed at any given location and that are the secondary--and,
therefore, far less fundamental--result of exceedingly complex resonant
processes acting on the traveling waves spawned by the primary tidal
interaction.=20
John
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A. John Mallinckrodt=A0=A0=A0=A0=A0
Professor of Physics=A0=A0=A0<mailto:ajmallinckro@csupomona.edu>mailto:ajmallinckro@csupomona.edu
Physics Department=A0=A0=A0=A0=A0=A0 voice:909-869-4054
Cal Poly Pomona=A0=A0=A0=A0=A0=A0=A0=A0=A0=A0=A0 fax:909-869-5090
Pomona, CA 91768-4031=A0=A0 office:Building 8, Room 223
=20