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milli360 wrote:
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I’ve given more detail in particular why no outward force is necessary. I’ve shown how centripetal acceleration, solar gravity and terrestrial gravity interact, and I’ve given you the tools to check the results for yourself. Does it help any or does it raise more problems? |
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milli360 wrote:
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However, since you ask, here a snip from Sawicki: '... there appears to be another force, the tidal force, pulling the mass m at points C and F up...' (Sawicki's emphasis), and one from the BA: 'It is mathematically correct to then subtract the force of the Moon on the center of the Earth from the force felt on the near and far sides. This is called vector addition. If we do that, our diagram will look like this: <- X -> far center near side of Earth side ' Not what I’d call explicit (that didn't print properly did it? - take a look at the BA home page). But I’m not much bothered about this, what concerns me most is that Sawicki’s paper totally ignores the centripetal acceleration of earths orbit. I’m frankly baffled that he should be so familiar with the suns gravitational gradient (D(a)s) yet (apparently) so ill informed about the complementary centripetal gradient. Replacing centripetal acceleration with ‘The Earth is simply in free fall towards the Sun’ is staggeringly naïve – it produces in a wrong explanation and it produces incorrect results. |
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That's fairly explicit, saying that gravity is the only force required. Quote:
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As someone said Einstein said, you want to make the theory as simple as possible, but no simpler. |
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OPPOSITE FACE LUNAR TIDAL BULGES ARE ELECTROSTATIC?
"Why is there a tidal bulge on the opposite side of the Earth?" Excellent question! But in reading the posts, I'm still not satisfied... In fact I've never found a truly satisfactory reason in all my readings why on the opposite side of the globe facing away from the moon or sun, are nearly the same as the tidal bulge facing them. The idea that the gravitational pull on the opposite side of the planet is canceled by the planet does not satisfy me. 'Push' gravity does not explain it effectively either, nor does the "three point pull". So I would like to present an idea which I suspect is original, if not crazy, though another may have thought of it first: the risen tide on the planet's opposite face away from the moon or sun is due to water's electrostatic charge. As outlandish as this may appear at first blush, consider the following suggestions: 1. There is a magnetic field from pole to pole, if off axis, that permeates the globe. This magnetic field gives a negative charge value to the northern hemisphere and a counter positive charge to the southern hemisphere, with a more neutral reading around the equator, where the positive and negative meet. 2. Tides appear to be greater towards the poles and lesser near the equator, which cannot be accounted by for planetary spin, since that would yield the opposite effect. So another cause must be found, which leads to the idea that like charges repel, even in the planet's ocean mass. 3. If like charges for large water mass, such as the oceans, repel, then the waters on the northern hemisphere, as they rise in response to the moon's or sun's gravity, will create a bulge towards the gravitational attraction and one opposite to it. This bulge creates a large negatively charged mass which, being of like charge, will be repelled on the opposite side of the planet, so that there too the water will bulge outwards. So due to like charge repelling like charge, the opposite side of the planet's mass is now counter-bulging in response to the mass bulge on the side facing the moon or sun. On the equator, where the positive-negative charge more or less cancels, there is less tidal opposite face response, so that there is less bulge than where the electrostatic charge is greater. On the southern hemisphere, the positively charged water mass likewise creates its own opposite bulge, same as in the northern. 4. Why does the equatorial water not bulge as much as towards the poles? My best guess is that it is already bulging, because of the planet's spin, so that the additional gravitational pull of the moon or sun does not displace this water as much as in either hemisphere because the centrifugal force already displaces it. Thus, equatorial waters should experience lower tides. I would expect, by this reasoning, that the waters near the artic or antartic circles should rise the most, and then taper off gradually towards the poles, or flatten out towards the equator. Of course, this basic principle is further modified by ocean currents and land mass interferences. So by this reasoning, the tidal bulges on the opposite side of the planet are actually electrostatic phenomena, where like charge repels like charge, even in the ocean waters. The same would be expected in the land mass, though to a much lower degree. In effect, the planet is pulsating with a gravitationally activated bulge which then triggers a like response on the opposite side of the planet through like electrostatic force repulsion. If this did not happen, the planet would wobble chaotically, which it does not. Pardon my ignorance, but I am not familiar with the above mentioned electrostatic theory of tides from any known sources, but would love to find out this it is not so. To my thinking, this much better explains why the tides create a like bulge on the opposite side of the planet, than any theory now found in existing textbooks. Blame it on the hot sun, but I got this idea while hiking up and down the rocky peaks near Pena Springs, Anza Borrego desert, last weekend, watching out for snakes and other prickly things. New barbs won't hurt me, so all challenges are welcome. 8) * * * * * (edited 3/18/04) * * * ... Having said all that, I must confess that this idea is really crazy, so ignore it... thanks. #-o
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‘Gravity cannot act in such a way as to make something feel a force away from an object.’ That would be explicit. Quote:
Is this what you are saying? I use w^2r to calculate centripetal acceleration and I don’t actually get that result, so (bearing in mind your quote of Einstein’s) could you maybe show your calculations, just for points O and F say. That would be most useful. Quote:
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But it’s an interesting subject and I’m keen to explore it further – anybody out there up for some sensible discussion? |
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The red dot is the center of the circle, and both orbit the red X. The circle does not rotate as it orbits, as can be seen from the orientation of the black dot at each step. The center of the black dot's orbit is the black X. The radius of the red dot's orbit is equal to the radius of the black dot's orbit. |
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Take point F, for example. Sometimes it is closer to the centre of the Sun, so gravitational acceleration is greater than centrifugal acceleration - hence there is a tidal bulge towards the Sun. At other times it is further from the Sun, so centrifugal acceleration is the greater - hence the tidal bulge away from the Sun.
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And so even if there were zero centrifugal acceleration (not orbiting, just falling), there would still be differences in gravitational acceleration, and the net difference would be the same as when orbiting, so the tidal forces - and thus, the tidal bulges - would be the same.
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I take it that you are still advocating for the differential orbits explanation, and you think it is similar to RichardMB's.
How does the DO explanation deal with the low tide on the side of the Earth? That question came up earlier. |
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Remember the tennis ball? Tie a string to it, dunk it in water again and whirl it round your head – what do you see happens to the water? It goes round to the far side, isn’t that right? This is another tidal bulge – a centripetal acceleration tidal bulge. Now ask yourself what possible difference will it make to this bulge if the ball were to rotate on its axis. Even if you’re unsure about centripetal acceleration you must surely realise that the balls own rotation doesn’t matter squat. The whole idea is just plain daft. So don’t analyse it – put it in the recycle bin. And don’t wait 2 years. ---------------- In astronomy, things are only as complicated as you care to make them. |
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In order to study the tidal bulge, you have to ignore that bulge, which is due to the rotation of the planet. As far as the tide is concerned, that flattening bulge is "squat", and you have to remove it from the calculations somehow. You have to treat the case of a non-rotating planet. |
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__________________
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I am not arguing that there are not alternatives to ways of explaining the tides--different reference frames can be effective. However, it's not as simple as it seems, and the BA's approach is not incorrect. PS: Here's a simplified calculation. At the center of the Earth, the acceleration due to the Sun's mass M is GM/R^2, where R is the distance to the Sun. At the far side of the Earth, the acceleration is GM/(R+r)^2, where r is the radius of the Earth. Subtracting the two gives GM(-2Rr-r^2)/(R^2 (R+r)^2), which is approximately -2GMr/R^3. That's in accord with the usual description of the tide-rasing force acceleration. At the points of low tide, the distance to the Sun is very nearly the same as at the center of the Earth, GM/R^2. That's the problem I've mentioned. However, the force of the Sun's gravity is not directed parallel to that at the center of the Earth. There are two components, one directed parallel, and one perpendicular, towards the center of the Earth. The right triangle has sides r and R. When you subtract the two, as vectors, then, the difference is r/R times GM/R^2, or GM/R^3. That's half of the tide-raising accleration calculated above--and that is what is found in the accelerometer data. The equipotential surface at low tide is depressed half as much as it is raised at high tide. |
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I just didn’t want you distracted by milli360’s diagram because it doesn’t correctly represent centripetal acceleration as it applies to tidal bulges. You can easily change the diagram so that it does though. Simply draw two circles (centred on the red cross) a big one of radius 1AU+R (R=earth radius) and a small one of radius 1AU-R. Label the big circle F and the small circle C. Circle F is the circle through which all the outer high tides pass, whilst circle C is the one through which all the inner high tides pass – they are, of course, coaxial. For a given angular velocity, the centripetal acceleration for path F is greater than for path C. From which it then follows that the centripetal acceleration at the outer bulge is constant and larger than the small constant centripetal acceleration at the inner bulge. To me this is so obvious but I’ve learned that it won’t be obvious to everyone. Does it make sense to you or do you have problems with it? |
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For a correct explanation however, you need to include centripetal acceleration, and for my money it’s also the simplest. |
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Just to follow up one of my previous posts. There is a derivation of the tidal potential that is presented in Stacey's Physics of the Earth (p115). It includes a once-per-revolution (once per year) rotation of the Earth, so it should satisfy your objections. After making the calculations and simplifying the algebra, Stacey comes up with a formula for the potential that includes three separate terms. The third term is - 1/2 w^2 r^2 sin^2 theta, where w is the rotation, r is the radius, and theta is the colatitude. It's the rotational potential due to the rotation, and it would contribute to the rotational potential if the rotation were much larger (once per day). If the problem were set up without that rotation, the algebra might be more difficult, but the answer would be the same, except this term would disappear. The first term is a constant, independent of position on the Earth, and, as Stacey says, "has no tidal effect." It's the gravitational potential at the center of the Earth due to the moon, with a small correction. The second term is the tidal potential, and is -Gmr^2/R^3 times (3/2cos^2 xi - 1/2), where xi is the angle off the line between the moon and Earth. That last factor is just a second order zonal harmonic, a prolate ellipsoid pointed at the moon.
The gradient of that tidal potential is the tidal force, and it is the same as that computed by the method of differential gravity that we've used above. It shows the depression of the low tide that seems to be missing from the differential orbit method. So, as I've said, it is possible to include all the terms in a system which includes a rotating earth and come up with the right answer, but you have to be careful--for instance, you have to identify, and then ignore, the bulge induced by that rotation. |
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My problem however isn’t with Stacey’s Physics of the Earth, it’s with Phil Plait’s Bad Astronomy, specifically this idea that the far tidal bulge is caused by differential gravity (attributed to Mik Sawicki). It isn’t – that’s Bad Physics. The far bulge would exist even if you removed the sun and its gravity completely, so long as earth’s orbital path was maintained. In fact the far bulge would then be an awful lot bigger. Putting the sun and its gravity back would actually depress the far bulge – exactly the opposite of what Sawicki suggests. Differential gravity can produce planet rupturing stresses, no doubt about that, but what differential gravity cannot do is induce any kind if push force. On it’s own solar gravity would pull all the oceans, and even the atmosphere, to the near side. To raise the far tide you need (and it is not optional) the centripetal acceleration of earth’s solar orbit. |
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And the interesting thing about it is that the centripetal component is also factored out--it's irrelevant as well. Quote:
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What I have not yet done is combine these two bulges. I don’t want to give the idea that you can simply stick these two bulges on the earth and get the high tides. It’s more complicated than that – but only a bit. |
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The point is, once you're done, you'll get the same answer that the BA gets--and his method is valid. It is not incorrect, as you claim. |
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