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uk.sci.weather (UK Weather) (uk.sci.weather) For the discussion of daily weather events, chiefly affecting the UK and adjacent parts of Europe, both past and predicted. The discussion is open to all, but contributions on a practical scientific level are encouraged. |
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#11
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Tides must have made colonisation of land by marine life a lot
easier.. First adapt to drying out part of the time. Richard Webb |
#12
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on a related topic see-
Title: What if the Moon didn't exist? Earths that might have been. http://www.atmos.ucla.edu/~fovell/AS19/index.html -- regards, david |
#13
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#14
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Mike Tullett wrote in message ...
Do you want to write to newsgroups and ask them to pull that bafflement before you get blinded by science? |
#15
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On 25 Sep 2003 18:41:24 -0700, Michael McNeil in
. com wrote: Do you want to write to newsgroups and ask them to pull that bafflement before you get blinded by science? I'd answer that question if I had the the first idea what you meant. I'm not baffled, as I taught *some* aspects of dynamic oceanography for over 20 years and thus claim some knowledge of the topic. -- Mike posted to uk.sci.weather 26/09/2003 08:15:20 UTC Coleraine Seeking information about the Internet and the way it works? - Subscribe to news:uk.net.beginners |
#16
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#17
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![]() "Mike Tullett" wrote in message ... On 25 Sep 2003 18:41:24 -0700, Michael McNeil in . com wrote: Do you want to write to newsgroups and ask them to pull that bafflement before you get blinded by science? I'd answer that question if I had the the first idea what you meant. I'm not baffled, as I taught *some* aspects of dynamic oceanography for over 20 years and thus claim some knowledge of the topic. Well it made reasonable sense to me..... Thanks. Col -- Bolton, Lancashire. 160m asl. http://www.reddwarfer.btinternet.co.uk |
#18
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Imagine having to bump into each other until they
developed eye sockets whilst on dry land. You've just described the average current-day driver ;-) ~~~~~~~~~~ This is sent from a redundant email Mail sent to it is dumped My correct one can be gleaned from h*$el***$$n*$d$ot$**s**i$$m*$m$**on**$s$@*$$a**$*o l*$*.*$$c$om*$ by getting rid of the overdependence on money and fame ~~~~~~~~~~ |
#19
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Mike Tullett wrote in message ...
I'm not baffled, as I taught *some* aspects of dynamic oceanography for over 20 years and thus claim some knowledge of the topic. So you have been teaching it as long as I have been trying to understand it? And this is not bull sh then: To understand the second bulge in the lunar component, we have to treat the earth and moon as one system with a common centre of mass. This is known as the Barycentre and lies within the earth, nearly 3000 miles from the earth's centre. Not only is the moon rotating about this point once very 28 days, but so is the earth's centre, i.e. it wobbles as it orbits the sun. One can argue to keep the earth rotating around that point, requires an inward acting force (on the opposite side to the moon - a centripetal force) and this weakens the "gravity" there thus allowing that second bulge to form. I am simplifying things a lot and diagrams would be useful. This site looks quite sound - "Why are there two high tides each day" http://www.math.nus.edu.sg/aslaksen/teaching/tides.html Mind you, this is very much the Newtonian approach and assumes very deep water (much deeper than is really the case), and no land to affect the tidal bulges as the encircle the earth. 1. First of all can we agree that due to the surrounding mass of the earth there is virtually no gravity or rather almost zero gravitational attraction at the centre of the earth? This being similar to what would happen to the smaller mass in a Cavendish gravity experiment if two equal weights were counterbalanced each side of it. (The centre mass is "not attracted to either." As it were) (And by extension showing that the tidal raising ability of the full moon is much less than at any other phase or portion of a phase.) 2. By further extension the barycentre is the centre of the sun, moon and earth. Therefore they will have no "pull" on an object at point zero. 3. The simplification of an inward acting force (if that were a possibility) requires that it is uni- or bi- directional in order to affect only one or two sides of the earth; yet we have shown that the barycentre is by definition a centre of gravity. As regards Newton, he did not resolve the problem of tidal action except that he acknowledged the seas only obeyed the perception in the Sea of Aethiope and nowhere else. Today of course we know that there are numerous varieties of tides from the one a day that follows the sun at Fiji, to the complex double highs of the Solent and the extraordinary ranges such as at Bristol. And that some tides, such as those at Seattle, have a mixed tropical and whatever the name for our type is. As it happens it appears that the tide around the British Islands seem to work on a three phase pulse where the tides at Orkney, Liverpool and Dover are nearly at high or low tide at the same time but those on the west of Ireland, Hull and Bristol are on the opposite part of the range. As for the rest of the stuff on that site I just get past boredom trying to put it all straight. You must choose to believe what you wish. I know I can't convince you otherwise. |
#20
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