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#1 |
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Join Date: Nov 2001
Posts: 2,281
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"Bad Astronomy" question re Earth and Moon
I've searched the web quite a bit but can't find answers to this. Maybe the BA or someone else knows. (Of course the BA knows!
)In Phil Plait's book, and on the BA website, we have this:
Quote:
Also, I seem to remember reading somewhere that the Earth will also eventually be locked with the same face towards the Sun. Again, does anyone know how long before this happens? Thanks |
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#2 |
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Thinker
Join Date: Jul 2002
Location: Canberra, Australia
Posts: 140
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The sort of time frame for the Earth to be tidally locked to the Moon is billions of years - roughly the same as the Main Sequence lifespan of the Sun.
In other words, some time between 1 and 10 billion years in the future, the Earth will become tidally locked with the Moon, and get toasted by the Sun. I don't think the Earth can become tidally locked with the Sun and the Moon, as this would require the Moon to take a year to orbit the Earth, and that doesn't sound possible. |
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#3 |
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Graduate Poster
Join Date: May 2003
Location: Canberra
Posts: 1,644
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I'm no scientition, but this doesn't sound right, the moon currently takes 28 days to orbit the earth, give or take. It is slowing the earth down to steal energy so it can recede further from the earth, thus taking even longer to orbit, so our days gradually get longer, the moon also orbits more slowley, I would have thought that it would escape earth orbit long before the days became like a month long. Or we get burned up by the sun before then aswell.
Like I said, just my opinion |
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__________________
Squishy doesn't irritate the hell out of me. - Quester_X |
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#4 |
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Guest
Posts: n/a
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Quote:
Tidal locking has to do with the fact that the tides are "dragged" behind the Earth's rotation, and eventually this dragging will slow the Earth's rotation. Admittedly, this will take billions of years. The Moon's orbital speed around the Earth is the primary reason for the receeding Moon. Since there are no tides on or in the Moon (that I'm aware of), the tidal dragging shouldn't affect the Moon's orbital speed at all. Also, tidal drag affects the rotational speed of the Earth with respect to the Moon. If there were tides on the Moon, they'd still not impact the orbital speed of the Moon at all. They'd only affect the Moon inasmuch as causing a force towards tidal locking with the Earth - a condition that already exists. The orbital speed remains unaffected. |
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#5 |
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Graduate Poster
Join Date: Jun 2003
Posts: 1,106
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Quote:
included below:Geostationary orbit (right now) is 35,786 km above the surface. The moon is 384,400 km above the surface. |
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__________________
Quality never goes begging. |
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#6 |
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Join Date: Nov 2001
Posts: 2,281
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#7 |
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Graduate Poster
Join Date: May 2003
Location: Canberra
Posts: 1,644
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I was taught at my amateur astronomy class, that the moon shows only one face to earth because it has a bulge, it is far from a sphere, or even a squashed sphere, there is a big lump on one side, and that means this lump gets locked facing earth, I believe it could also get locked facing away but the lump ended up pointed towards earth.
I was also taught it was receding, because if the earth is slowing down from tidal drag, the energy must be transferred somewhere, it doesn't just go away, so it goes to the moon, which then recedes. As for the eventually only showing one face to the moon like I said earlier, the earths day would have to slow down to be in excess of 28 current days (672 hours), now they reckon when the moon first formed the earths day was like 4 hours long, but as the moon recedes the rate of slowing recedes. So we are rotating 6 times slower than when the moon first appeared, and the effect of moons slowing is GREATLY reduced now than when it first appeared, and we would have to slow down a further 28 times for this to happen. Is there enough time for this even assuming we freeze the sun so it doesn't kill the whole thing, would not the moon leave before this could happen? Anyone? |
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__________________
Squishy doesn't irritate the hell out of me. - Quester_X |
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#8 |
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Join Date: Nov 2001
Posts: 2,281
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Quote:
Quote:
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#10 |
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NLH
Join Date: Oct 2002
Posts: 25,907
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About 30 years ago, (back in the Pliocene), I read a paper by (I think) Moorbath & Runcorn on Growth structures of Devonian Corals which indicated a 400 day (tide) year. The cause was theorised to be the smaller diameter of the Earth - Moon system. There were one or two inconsistencies with the model, as pushing it back in time seemed to imply far higher tidal ranges, while other fossil data (Stromatolites and banded Ironstones) implied a smaller tidal range for the precambrian.
Anyone read anything more up to date on the question? Nb. There are tides on the Moon. They are Earth (oops) Moon tides. Not so obvious as sea tides, but quite real. |
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