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- From: jbh55289@uxa.cso.uiuc.edu (Josh 'K' Hopkins)
- Subject: Re: ROTATION OF THE MOON
- References: <1992Nov18.163804.1213@sunspot.noao.edu> <1992Nov19.144441.5498@col.hp.com> <1992Nov19.220246.6719@u.washington.edu>
- Message-ID: <By1AC5.Kts@news.cso.uiuc.edu>
- Sender: usenet@news.cso.uiuc.edu (Net Noise owner)
- Organization: University of Illinois at Urbana
- Distribution: na
- Date: Fri, 20 Nov 1992 21:28:52 GMT
- Lines: 24
-
- labmas@stein.u.washington.edu (Michael Andersson) writes:
-
- >In article <1992Nov19.144441.5498@col.hp.com> dag@col.hp.com (David Geiser) writes:
- >>> The same thing is happening, much more slowly, to the earth --
- >>> friction with the tides and within the "solid" earth is slowing the
- >>> rotation rate by something on the order of 1 sec every century. We can
- >>> actually measure it (the slowdown) nowadays. Love those atomic clocks!
- >>
- >>Do you know if that rate is constant? Say around 63M years ago,
- >>around the time of the end of the dinosaurs, the day would have
- >>been 175 hrs longer!
-
- >No. If the rotation is slowing, then days used to be shorter.
-
- Right, so the rate obviously isn't constant or the Earth would have been
- spinning at relativistic speeds shortly before our astraulopithic ancestors
- appeared. Since the rates depends on tides and gravitational fields it's very
- likely that there are exponential terms in the equation. If I recall correctly,
- you have cubics in the formula for tidal forces, which results in a much
- different curve than trying to plot it linearly.
- --
- Josh Hopkins jbh55289@uxa.cso.uiuc.edu
-
- "Why put off 'til tomorrow what you're never going to do anyway?"
-