Article View: alt.sci.planetary
Article #80Re: History of Earth/Moon system
From: Donald Banfield
Date: Wed, 06 Jan 1993 20:35
Date: Wed, 06 Jan 1993 20:35
47 lines
2915 bytes
2915 bytes
I just used or libraries computers to see if there was some recent stuff on lunar orbital changes due to tides. I found a couple of articles that seemed like they're worth checking out: Cheng, MK, Eanes, RJ, & Tapley, BD, Tidal Deceleration of the Moons Mean Motion, Geophysical Journal International, v.108, p.401-409 Dehant, V, Review or the Earth Tidal Models & Contribution of Earth Tides in Geodynamics, JGR-Solid Earth, v.96, p.235-240. Williams, GE, Tidal Rhythmites - Key to the History of the Earths Rotation and the Lunar Orbit, Journal of Physics of the Earth, v.38, p.475-491 This last one discusses paleo-evidence of the lunar period, probably more what you wanted... sounds like the lunar recession may have speeded up a bit around now, maybe a factor of 2 slower 600Ma ago. I've heard of this before, and I dimly recall speculation that it was a resonance in the ocean tides with their basin sizes. I'm sure you're aware that they're now directly measuring the lunar recession speed with laser ranging. This is what is compared with the paleo-evidence. If you know the distance to the moon, you can calculate the rotation rate of the Earth, assuming that the angular momentum of the Earth-moon system hasn't changed over the time-scale you're considering. I don't think I'd ascribe much depth to the similarity of Press & Siever's 11hr day being like the rotation rates of Juptier or Saturn. I think that most people feel that the moon was somehow created in some sort of a cataclysmic event with the earth, which would have significantly altered the angular momentum of the system from what it may have been primordially. On the other hand, there is a theory regarding the rotation rates of primordial bodies, but I'm not knowledgeable enough to even hazard a description of it here. Jack Lissauer and (separately, I believe) Luke Dones & Scott Tremaine have worked on it. Look for some recent papers of theirs. As far as how tidal recession is a function of distance from the central body, I'd look at a few papers by Peter Goldreich. Namely the bunch from around 1965. He derives the tidal changes there. He also wrote a paper, around 1967 that discussed the tidal history (and future?) of the moon. Try Q Values in the Solar System, Icarus v.5, p.375-389... I hope these ramblings help.... Don Banfield Caltech Planetary Science djb@cluster.gps.caltech.edu
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Path: arc1-ca.pugleaf.net!sparky!uunet!europa.asd.contel.com!darwin.sura.net!sgiblab!adagio.panasonic.com!nntp-server.caltech.edu!cluster.gps.caltech.edu!djb From: djb@cluster.gps.caltech.edu (Donald Banfield) Newsgroups: alt.sci.planetary Subject: Re: History of Earth/Moon system Date: 6 Jan 1993 20:35:55 GMT Organization: California Institute of Technology, Pasadena Lines: 49 Message-ID: <1iffrbINNs25@gap.caltech.edu> NNTP-Posting-Host: cluster.gps.caltech.edu