MadSci Network: Astronomy |
The centre of mass of the Earth-Moon system is quite easy to calculate. You just have to find the point where is the two bodies were connected by a rigid rod, they would balance. The Earth is about 1/80th the mass of the Earth so the point at which they would balance is about 1/80th of the distance from the Earth to the Moon. Since this is about 250,000 miles, the balance point (centre of mass) is just below the surface of the Earth on the side of the Earth facing the Moon. The Earth is indeed slowing down due to tidal friction. We are all familiar with water tides - but the same effect is going on within the solid Earth too and indeed the Earth raises much larger solid tides on the Moon (which have already stopped the rotation of the Moon relative to the Earth). As the Earth rotates, there is a friction which is slowing it down. Similarly this tidal friction affects the Moon and due to a physical law called the conservation of angular momentum, the Moon is actually getting further away from us, it used to be much closer in the past. This means that tidal friction is gradually slowing too so that it is not a simple matter to calculate how long it will take the Earth to slow down completely. In fact the best and most sensitive method of measuring how much the Earth is slowing down is to predict when and where total eclipses of the Sun (by the Moon) would have occurred in the past (over the past few thousand years). Ancient records tell us where the eclipse was actually seen - on the right predicted day but in the wrong place. That's because the Earth has slowed down just a little in that time and the cumlulative effects over so many rotations over a couple of thousand years throw off the calculated position by hundreds of miles. From this a very accurate figure for the slowing down can be determined.
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