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Natural Science Forum / Earth Science / Oceanography / September 2005



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Tides

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Michael Mcneil - 17 Jan 2005 08:23 GMT
Tides, Seiches, River Bores, Storm Surges and Tidal Waves.

Johannes Keppler and Gallileo Gallilei once argued over whether the moon
was the main cause of the tides. Whilst massive assumptions that don’t
stand up to any scrutiny are applied in the description of how the moon
is involved with the tides, no lien is given to the existence of any
input from the moon in the other phenomenae.

The accepted theory of lunar influence on tides is that the moon “raises
small particles” which tend to follow it. Meanwhile over on the other
side of the planet these particles, flowing away from the altazimuth,
cause high tides on that side of the earth at the same time.

Discrepancies in the observed times of high tide are explained as
friction.

Some obvious problems with this theory:

1. On the opposite side of the earth when these tides are supposed to
occur “by default” as it were, the tides are often a little higher than
those upon which the moon is alledged to have a direct bearing.

2. The direct gravity idea should show that the highest tides tend to
occur over the tropics, certainly at no time should they fail to form
highest peaks and troughs at greater latitudes than 28 north or south.
In these lower latitues both the sun and the moon are overhead.

3. In winter, the times of sunrise vary by many hours when compared to
the times of sunrise in summer. The time of moonrise varies even more
wildly EVERY MONTH not every year.

4. Water, even sea water, is considered a nearly perfect fluid.

5. According to the Cavendish experiment, the moon should (if the above
silliness hold true) attract heavier particles with more “alacrity” than
it does air and seawater. And of course it should show peaks in the
atmosphere far greater than is the present case. (The tropopause is
higher in lower latitudes due to the temperature. At least the
differences involved are more easily equated to that. For with the above
silliness, the upper atmosphere should be 1/80th of the distance to the
moon.)

The renaissance is generally counted as to have started some time around
the era in which Johannes Keppler and Gallileo Gallilei lived. The times
before then are sometimes spoken of as the dark ages, when natural
phenomenae were ascribed to supernatural causes. We can now explain most
of them in terms of schoolboy phyics. We believe we now live in an age
of reason and light.

It would seem we are still stumbling blindly in the dark over more than
a few things.
Robert Grumbine - 18 Jan 2005 20:56 GMT
>Tides, Seiches, River Bores, Storm Surges and Tidal Waves.
>
[quoted text clipped - 11 lines]
>Discrepancies in the observed times of high tide are explained as
>friction.

 I don't know where you got this from, but it's quite incorrect.
The main element for the age of the tide (difference between time
of overhead or directly opposite moon and high tide) is the limit
in ocean wave speed relative to the motion of the moon.  Ocean waves
propagate at ca. 200 m/s while the apparent motion of the moon
is ca 450 m/s (at the equator).  

 For a reasonable discussion of the tidal force and ocean response,
see, for example, Gill, A. E., Atmosphere-Ocean Dynamics, Academic
Press, 1982.

[snip]

>It would seem we are still stumbling blindly in the dark over more than
>a few things.

 But if you look to sources of illumination, you'll do better.

Signature

Robert Grumbine http://www.radix.net/~bobg/ Science faqs and amateur activities notes and links.
Sagredo (Galileo Galilei) "You present these recondite matters with too much
evidence and ease; this great facility makes them less appreciated than they
would be had they been presented in a more abstruse manner." Two New Sciences

PDQDL - 19 Jan 2005 23:46 GMT
> >Tides, Seiches, River Bores, Storm Surges and Tidal Waves.
> >
[quoted text clipped - 29 lines]
>
>   But if you look to sources of illumination, you'll do better.

A simpler explanation can be found in a bottle of pancake syrup.

Tip it over: observe why it there is a delay in reaching the maximum or
minimum tide levels.
Michael Mcneil - 19 Jan 2005 23:48 GMT
> >Discrepancies in the observed times of high tide are explained as
> >friction.

>   I don't know where you got this from, but it's quite incorrect.
> The main element for the age of the tide (difference between time
> of overhead or directly opposite moon and high tide) is the limit
> in ocean wave speed relative to the motion of the moon.  Ocean waves
> propagate at ca. 200 m/s while the apparent motion of the moon
> is ca 450 m/s (at the equator).  

It is based on an essay in the Encyclopeadia Britannica 1986 edition
discussing the work of George Darwin.

The actual method for forcasting tides can not be done using theory.
What is done is that a series of reading is taken over an year and the
immediate future obtained by interpolation. Most of the cheaper
programmes use a plot taken from the last month.

For a similar explanation you may want to check out Reeds or the Silk
Cut nautical almanacks. Along with the mumbo jumbo accepted at present
their is a lot of really useful information for those that have to
actually do something with the academical sh.t.
Michael Mcneil - 24 Jan 2005 05:22 GMT
There are about 46 "Primary Ports" along the coasts around the British
Isles for which the tidal tables have been worked out and which are
regularly updated.

The secondary ports appear in major shipping catalogues (called
almanacs) as river mouths at smaller towns, for which a process of
interpolation or exrapolation (I can never remember which is which) is
supplied as ready reckoners.

Other places along coasts can be guesstimated from those.

There are regions (such as the Fenns and the Menai Straights) for which
a consumate treatise is elusive. Such places, if they are important
industrially (as for example the river Dee, which has a rapidly changing
sand bar system that despite constant effort from dredgers and the like
really do need local knowledge) require piloting facilities.

The primary ports are:

Falmouth Devonport, & Dartmouth.
Portland, Poole, Southhampton & Portsmouth.
Shoreham & Dover.
Shhernes, London Bridge, Walton on Naze & Lowestoft.
Immingham & Tyne.
Leith & Aberdeen.
Lerwick.
Ullapool & Oban.
Greenock.
Liverpool & Holyhead.
Milford Haven & Avonmouth.
Dublin & Cobh.
Belfast & Galway.
Esbjerg.
Heligoland, Cuxhaven & Wilhelshaven.
The Hook of Holland & Vissingen.
Dieppe, Le Havre & and Cherbourg.
San Malo.
Saint Peter Port & Saint Helier.
Brest.
Nil
Pointe de Grave
Lisboa
Gibraltar.
Michael Mcneil - 24 Jan 2005 13:59 GMT
> There are about 46 "Primary Ports" along the coasts around the British
> Isles for which the tidal tables have been worked out and which are
> regularly updated.

See more on this at:
http://www.bbc.co.uk/weather/coast/tides/southwest.shtml

Another page on the BBC web site has this to on the construction of tide
tables:

The tides are generated by gravitational influences of the
Earth-Moon-Sun system, whose astronomical relationship and orbital
details are known extremely accurately. Using this information, together
with the tidal constants derived from the tidal analyses, the tides can
be predicted for any date as far ahead into the future as required.

However, for predictions well into the future (many decades) the effects
of global sea level rises and changes in seabed topography have to be
carefully considered. These may have a significant effect upon local
tidal behaviour, and the predictions can only be computed using the
tidal data currently available on the UKHO database. So the further
ahead we go from the date the tidal data is held on the database, the
less reliable the predictions will become.

You only have to note the changes in the table of lunar phases over a
period of less than an year to realise there is a degree of not
quiteness about the  above.
http://aa.usno.navy.mil/data/docs/MoonPhase.html#y2005

Only minor changes but they are there. As it happens the BBC is a noted
pander to accepted academic explanation. But that is just my personal
opinion. Don't let my disgust with them throw you off. See for yourself
if you agree with them:
http://www.bbc.co.uk/weather/features/coast_sea/tidesfaq.shtml

Here is a list of lunar phases for 2005. If I can find this thread in an
year's time (I will have forgotten all about it long efore then I
imagine) I shall post the same table for comparison.

NEW MOON    FIRST QUARTER        FULL MOON     LAST QUARTER

      d  h  m          d  h  m          d  h  m          d  h  m

                                                  JAN.   3 17 46
JAN.  10 12 03   JAN.  17  6 57   JAN.  25 10 32   FEB.   2  7 27
FEB.   8 22 28   FEB.  16  0 16   FEB.  24  4 54   MAR.   3 17 36
MAR.  10  9 10   MAR.  17 19 19   MAR.  25 20 58   APR.   2  0 50
APR.   8 20 32   APR.  16 14 37   APR.  24 10 06   MAY    1  6 24
MAY    8  8 45   MAY   16  8 56   MAY   23 20 18   MAY   30 11 47
JUNE   6 21 55   JUNE  15  1 22   JUNE  22  4 14   JUNE  28 18 23
JULY   6 12 02   JULY  14 15 20   JULY  21 11 00   JULY  28  3 19
AUG.   5  3 05   AUG.  13  2 38   AUG.  19 17 53   AUG.  26 15 18
SEPT.  3 18 45   SEPT. 11 11 37   SEPT. 18  2 01   SEPT. 25  6 41
OCT.   3 10 28   OCT.  10 19 01   OCT.  17 12 14   OCT.  25  1 17
NOV.   2  1 24   NOV.   9  1 57   NOV.  16  0 57   NOV.  23 22 11
DEC.   1 15 01   DEC.   8  9 36   DEC.  15 16 15   DEC.  23 19 36
DEC.  31  3 12
Michael Mcneil - 07 Feb 2005 06:38 GMT
Lunar Tides

I have a copy of the Encyclopaedia Britannica but it will not work with
XP or for some yet to be resolved problem. So some commuting -as and
when
possible, to my local library is required. It is 3:15 (and counting) on
Monday morning so that is out of the question for a few hours.

This is the standard newbie level of understanding of tides aka Encarta:

The Moon, being much nearer to the Earth than the Sun, is the principal
cause of tides. When the Moon is directly over a given point on the
surface of the Earth, it exerts a powerful pull on the water, which
therefore rises above its normal level. Water covering the part of the
Earth farthest from the Moon is also subject to this pull, so that
another distinct dome of water is formed on the farther side of the
Earth providing the basis for a second wave. The lunar wave crest
directly beneath the Moon is called direct tide, and the crest on the
side of the Earth diametrically opposite is called opposite tide. At
both crests, the condition known as high water prevails, while along the
circumference of the Earth perpendicular to the direct-opposite tidal
axis, phases of low water occur.

Low and high waters alternate in a continuous cycle. The variations that
naturally occur in the level between successive high water and low water
are referred to as the range of the tide. At most shores throughout the
world, two high waters and two low waters occur every lunar day, the
average length of a lunar day being 24 hr, 50 min, and 28 sec. One of
these high waters is caused by the direct-tide crest and the other by
the opposite-tide crest. Two successive high waters or low waters are
generally of about the same height. At various places outside the
Atlantic Ocean, however, these heights vary considerably; this
phenomenon, which is known as diurnal inequality, is not completely
understood.

http://uk.encarta.msn.com/encyclopedia_761561041/Tide.html#endads
Michael Mcneil - 07 Feb 2005 07:08 GMT
Newton's Three  Laws of Motion

Newton's first law of motion states that if all the forces acting on an
object is zero, then the object will remain at rest or remain moving at
constant velocity.

The Second Law

Newton's second law relates net force to acceleration. A net force on
an object will accelerate it —that is, change its velocity.

The acceleration will be proportional to the magnitude of the force and
in the same direction as the force. The proportional constant is the
mass, m = F/a

A more massive object will require a greater force for a given
acceleration than a less massive one.

The Third Law

Newton's third law of motion states that when an object exerts a force
on another object, it experiences a force in return. The force that
object 1 exerts on object 2 must be of the same magnitude as the force
that object 2 exerts on object 1 but in the opposite direction.

http://uk.encarta.msn.com/encyclopedia_761556906/Mechanics.html

Or to put that last bit in perspective:

Newton's third law of motion states that when an object exerts a force
on another object, it experiences a force in return.

The force that the moon exerts on a drop of water must be of the same
magnitude as the force that a drop of water exerts on the moon but in
the opposite direction.
Simon Waldman - 07 Feb 2005 09:28 GMT
> Newton's third law of motion states that when an object exerts a force
> on another object, it experiences a force in return.
>
> The force that the moon exerts on a drop of water must be of the same
> magnitude as the force that a drop of water exerts on the moon but in
> the opposite direction.

Correct.

A drop of water is small and light, so that force can move (well,
accelerate) it a lot.

The Moon is large and heavy, so the same force doesn't have much effect.

Signature

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Hatunen - 08 Feb 2005 18:46 GMT
>Lunar Tides
>
[quoted text clipped - 10 lines]
>surface of the Earth, it exerts a powerful pull on the water, which
>therefore rises above its normal level.

Actually, the gravitational field of the sun is far larger at the
earth than is the moon's. The tides are not due to the *strength*
of the gravitational field, but rather the gradient of the field.

>Water covering the part of the
>Earth farthest from the Moon is also subject to this pull,

Eh?

>so that
>another distinct dome of water is formed on the farther side of the
[quoted text clipped - 18 lines]
>
>http://uk.encarta.msn.com/encyclopedia_761561041/Tide.html#endads

Issac Newton originally explained the tides, but it appears the
writers and ediors of Encarta didn't bothe to check on good old
Ike; i.e., Encarta got it wrong, wrong, wrong.

See http://csep10.phys.utk.edu/astr161/lect/time/tides.html for a
correct, if simplified, explanation.

I've seen the Britannica explanation and it is correct.

   ************* DAVE HATUNEN (hatunen@cox.net) *************
   *       Tucson Arizona, out where the cacti grow         *
   * My typos & mispellings are intentional copyright traps *
Michael Mcneil - 08 Feb 2005 18:44 GMT
> Issac Newton originally explained the tides, but it appears the
> writers and ediors of Encarta didn't bother to check on good old
> Ike; i.e., Encarta got it wrong, wrong, wrong.

Actually Newton failed to explain it and no-one since has come up with
the answer either. Lord Kelvin came up with the tidal calculator but it
is not an explanation of tides.

> See http://csep10.phys.utk.edu/astr161/lect/time/tides.html for a
> correct, if simplified, explanation.

Why the link -which also fails masterfully btw, has to work with San
Fransisco and Galveston (some 35 degrees apart) when the more acceptable
division is New Orleans, Fiji, Calcutta and Portsmouth (all some 90
degrees apart) is beyond me

New Orleans has diurnal tides I believe. The links both describe a
semidiurnal. No idea how the bulge on the far side is caused. That was
the main point of the original post by the way.

It doen't fit the basic physics on which the universe runs.

Fiji's tides are timed to the sun.

Portsmouth has a double high and low water. How is that due to the
moon?

How is the fact that the tides one end of the channel it is in the
middle of, can have high tide when the other end has low tide if the
link is correct?

> I've seen the Britannica explanation and it is correct.

I finally got my disk working but I can't take to the interface at all.

Sooooo
It's back to the library.
Simon Waldman - 08 Feb 2005 19:27 GMT
> Portsmouth has a double high and low water. How is that due to the
> moon?

I can't answer most of the rest of this post. But the reason that the
Solent (the area between the Isle of Wight and the mainland) gets double
tides is simply that the "surge" of water that is making its way along
the English Channel enters the Solent from one end and then, a couple of
hours later, also enters the Solent from the other end.

Or at least, that's how I've always understood it. It makes intuitive
sense to me.

Followups set to sci.geo.oceanography, as this has sod all to do with
earthquakes.

Signature

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SteveR - 09 Feb 2005 13:36 GMT
The tide are measured at a location and the data is analised using FFT
to produce the tidal harmonics. This separates the different inflences
on the tides such as S2 being the larger tidal input of the sun and M2
being the same for the moon. It should be noted that although M2 is the
most important tidal input for most of the world. there are some places
where the solar input is actually greater. I have always understood
these differences to be due to Amphidromic systems where the "wave" of
the tide, when nearing a coast would rotate around a point so that
tidal times are defined by that arrangement more than the simle moon
-sun orientation.

Feel free to correct me if I am wrong. I have none of my papers with me
and mearly remembering college 7 years ago.

Stephen Redford
Michael Mcneil - 10 Feb 2005 06:51 GMT

> > Portsmouth has a double high and low water. How is that due to the
> > moon?

> I can't answer most of the rest of this post. But the reason that the
> Solent (the area between the Isle of Wight and the mainland) gets double
> tides is simply that the "surge" of water that is making its way along
> the English Channel enters the Solent from one end and then, a couple of
> hours later, also enters the Solent from the other end.

You can't answer this one too neither, since it requires you to denounce
the "fact" that a pull causes a surge that ddrags water thither and yon.

> Or at least, that's how I've always understood it. It makes intuitive
> sense to me.

Intuitive sense. Isn't that the reason most gullible or ignorant people
presume they understand most things? Not least among those, the tides.

> Followups set to sci.geo.oceanography, as this has sod all to do with
> earthquakes.

Actually this has quite a lot to do with earthquakes not least of the
reasons being the ignorance among the regulars there about tides.

"SteveR" <s.redford@gmail.com> wrote in message
news:1107956169.429456.238110@l41g2000cwc.googlegroups.com

> The tide are measured at a location and the data is analysed using FFT
> to produce the tidal harmonics. This separates the different influences
> on the tides such as S2 being the larger tidal input of the sun and M2
> being x for the moon. It should be noted that although M2 is the
> most important tidal input for most of the world, there are some places
> where the solar input is actually greater.

Could you explain the terms FFT and Amphidromic for the sake of those
whose half open minds are already jading shallowly?

> I have always understood
> these differences to be due to Amphidromic systems where the "wave" of
> the tide, when nearing a coast would rotate around a point so that
> tidal times are defined by that arrangement more than the simple moon
> -sun orientation.

I posted a pic of co-tidal lines here:

http://groups.msn.com/Weatherlore/general.msnw?action=get_message&mview=0&ID_Mes
sage=268


Most library hubs in the UK will have a decent enough reference centre
to get a look at books on the subject. Wouldn't you know it but my biro
ran out when I was writing the source for the photocopy.

Introduction to Physical and Biologic(al?) Ocean.........??

By ....? King.

> Feel free to correct me if I am wrong. I have none of my papers with me
> and merely remembering college 7 years ago.

I'm zenning most of this too. Intuitively? I haven't the access to the
books I once had. Mind you it's been interesting relearning it all
again.

Sorry to have to post your reply with the dimmo's but if you wanted to
have this discussion with me it had to be with the input going to both
groups. If you and dickhead up there^ don't like it, then start your own
thread.
Simon Waldman - 10 Feb 2005 10:47 GMT
>>Michael Mcneil wrote:

>>>Portsmouth has a double high and low water. How is that due to the
>>>moon?
[quoted text clipped - 7 lines]
> You can't answer this one too neither, since it requires you to denounce
> the "fact" that a pull causes a surge that ddrags water thither and yon.

I'm sorry, but I don't understand your sentence. If you can rephrase it
comprehensibly I'll endeavour to respond.

>>Or at least, that's how I've always understood it. It makes intuitive
>>sense to me.
>
> Intuitive sense. Isn't that the reason most gullible or ignorant people
> presume they understand most things? Not least among those, the tides.

Possibly. That doesn't mean it has to be wrong.

>>Followups set to sci.geo.oceanography, as this has sod all to do with
>>earthquakes.
>
> Actually this has quite a lot to do with earthquakes not least of the
> reasons being the ignorance among the regulars there about tides.

The regulars of sci.geo.earthquakes being ignorant about tides does not
make a discussion of tides relevant to sci.geo.earthquakes. I am quite
ignorant of cookery, but that doesn't mean that people should crosspost
about cookery into unrelated groups that I frequent.

I'm sure that if people from sci.geo.earthquakes want to learn about
tides and other topics related to oceanography, they are quite capable
of subscribing themselves to sci.geo.oceanography.

<snip of what seems to be a reply to somebody else's post, appended to
the end of this post for no immediately obvious reason>

-Simon.

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Hatunen - 10 Feb 2005 16:39 GMT
>The regulars of sci.geo.earthquakes being ignorant about tides does not
>make a discussion of tides relevant to sci.geo.earthquakes. I am quite
[quoted text clipped - 4 lines]
>tides and other topics related to oceanography, they are quite capable
>of subscribing themselves to sci.geo.oceanography.

The tides are relevant to sci.geo.earthquakes if you wish to
address the common claim that earthquakes can be caused by the
alignment of earth, moon and sun, so you might suspend your
snottiness accordingly and find other windmills to tilt at.

   ************* DAVE HATUNEN (hatunen@cox.net) *************
   *       Tucson Arizona, out where the cacti grow         *
   * My typos & mispellings are intentional copyright traps *
Michael Mcneil - 11 Feb 2005 13:24 GMT
> The tides are relevant to sci.geo.earthquakes if you wish to
> address the common claim that earthquakes can be caused by the
> alignment of earth, moon and sun, so you might suspend your
> snottiness accordingly and find other windmills to tilt at.

My reasoning too. The twit is probably just miffed that no-one ever
posts to sci.geo.oceanography.

Besides the chat on sci.geo.earthquakes recently was full of stuff about
tidal waves. Concerning which I have yet to see a scientific explanation
about why the shock did not induce more chaotic splashing instead of the
cohesive system that was invoked.

What sort of discussions were they? Nothing but bickering over words.

And were there a higher class of discussion about tidal waves in any of
the myriad threads on sci.geo.oceanography?

Speaking of which, just what sort of posts has the twit posted there?

I don't remember coming across anything of any calibre.
Simon Waldman - 11 Feb 2005 15:24 GMT
>>The tides are relevant to sci.geo.earthquakes if you wish to
>>address the common claim that earthquakes can be caused by the
>>alignment of earth, moon and sun, so you might suspend your
>>snottiness accordingly and find other windmills to tilt at.
>
> My reasoning too.

I stand corrected. My apologies to anybody who I offended.

I felt that I would be doing a good turn by setting followups, as I
didn't see that what I was writing (about my understanding of tides in
the Solent) had any relevance to earthquakes, and did so.

I happened to be feeling rather irritable at the time that I received
the reply to this, and since the reason given for the relevance of the
crossposting was a nonsensical one (something that I still believe), I
was overly sarcastic. This was, indeed, uncalled for.

> The twit is probably just miffed that no-one ever
> posts to sci.geo.oceanography.

Assuming that "the twit" refers to me: Not at all. I am generally a
lurker on s.g.o, and even though it is a low-traffic group I learn a
great deal from the few posts that do appear.

> Speaking of which, just what sort of posts has the twit posted there?
>
> I don't remember coming across anything of any calibre.

Indeed not. I mostly lurk there as I'm no great expert on the matters
discussed.

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Felix Tilley - 11 Feb 2005 17:07 GMT

> I stand corrected. My apologies to anybody who I offended.

You are replying to one of sci.geo.earthquakes resident k00ks.  KF McNeil.  
Lossless compression.  And don't worry about offending him.
Michael Mcneil - 12 Feb 2005 05:59 GMT
> My apologies to anybody who I offended.

No need to appologise there are a lot worse things going on in sge.

Being one of the main culprits I tend to behave rather worse than most.
No excuses though and no appologies too, neither.

I have come across a nice essay on the subject of tides in the book I
stole the reproduction of co-tidal lines from:

Introduction to Physical and Biological Oceanography.

I'll post more later. Most of it is repeated in a slightly more
concise form in Brown's Nautical Almanac (I doubt it is still in
production these days with satellite navigation and global communication
as well as computed data so readily available.)

The gist is still the same though. (It's just the sightings tables have
gone with the sextant, making the need for a new text book each year
unecessary.)

I am sorry I am so churlish. I keep meaning to change but I can't be
bothered.
Michael Mcneil - 12 Feb 2005 06:14 GMT
Introduction to Physical & Biological Oceanography
ISBN: 0844804002
Author: Cuchlaine King  
Hatunen - 08 Feb 2005 22:23 GMT
>> Issac Newton originally explained the tides, but it appears the
>> writers and ediors of Encarta didn't bother to check on good old
[quoted text clipped - 3 lines]
>the answer either. Lord Kelvin came up with the tidal calculator but it
>is not an explanation of tides.

Oh, dear. Most of us who studied physics have always assumed Ike
got it right. Not least because we're able to perform the same
rather trivial calculations he used. What part do you claim he
got wrong and/or what is the correct explanation?

   ************* DAVE HATUNEN (hatunen@cox.net) *************
   *       Tucson Arizona, out where the cacti grow         *
   * My typos & mispellings are intentional copyright traps *
Michael Mcneil - 08 Feb 2005 23:57 GMT
> Oh, dear. Most of us who studied physics have always assumed Ike
> got it right. Not least because we're able to perform the same
> rather trivial calculations he used. What part do you claim he
> got wrong and/or what is the correct explanation?

Ike?

I was talking about Isaac Newton. If you remember reading his book, he
did
admit that the calculations he was using could not explain the behaviour
of tides except for the Aethiope Sea. ISTR he only said a part of that
too.

I do have a link to Pricipia online but AOL is playing silly buggers
with my links at the moment. Nothing stopping you from looking for one
though. I can't quote you chapter and verse but a re-read is always
worthwhile with such a masterpiece of logic.

Have fun.
Hatunen - 09 Feb 2005 01:33 GMT
>> Oh, dear. Most of us who studied physics have always assumed Ike
>> got it right. Not least because we're able to perform the same
[quoted text clipped - 13 lines]
>though. I can't quote you chapter and verse but a re-read is always
>worthwhile with such a masterpiece of logic.

You may have noticed that the Encarta article I was responding to
addresssed the general theory of the tides, not the specific
locational variances. And Newton was quite correct in his general
theory of the tides and Encarta is wrong.

   ************* DAVE HATUNEN (hatunen@cox.net) *************
   *       Tucson Arizona, out where the cacti grow         *
   * My typos & mispellings are intentional copyright traps *
Michael Mcneil - 10 Feb 2005 06:59 GMT
> You may have noticed that the Encarta article I was responding to
> addresssed the general theory of the tides, not the specific
> locational variances. And Newton was quite correct in his general
> theory of the tides and Encarta is wrong.

Here is the link I have:
http://members.tripod.com/~gravitee/toc.htm
Search for yourself and see what he had to say about tides.

Make sure you have your pop-up controls switched on as it is a really
drech site, full of banners and pop up crapware.
Hatunen - 10 Feb 2005 16:36 GMT
>> You may have noticed that the Encarta article I was responding to
>> addresssed the general theory of the tides, not the specific
[quoted text clipped - 4 lines]
>http://members.tripod.com/~gravitee/toc.htm
>Search for yourself and see what he had to say about tides.

Unfortunately, it does not appear anything in that link addresses
the tides, the tides appearing in Book II.

   ************* DAVE HATUNEN (hatunen@cox.net) *************
   *       Tucson Arizona, out where the cacti grow         *
   * My typos & mispellings are intentional copyright traps *
BSquared - 09 Feb 2005 02:27 GMT
"Up antenna!"

Mike!  I don't mean to flame you.  But, in the below discussion you mention
that New Orleans might be a good place from which to compare tide
generation.

FYI:  The tides in New Orleans are so controlled by the Mississippi River
that NOAA (the Natioanl Oceanic and Atmospheric Administration, an agency
within the U.S.Department of Commerce) does not have a tide gage at New
Orleans. Nor do they publish predictions or actual water levels for N.O.
The closest tide gage is many miles south of New Orleans at Southwest Pass
in the Mississippi delta.  New Orleans is on the Mississippi River not on
the Gulf of Mexico.

For a rather good explanation of tidal forces, go to:

http://www.co-ops.nos.noaa.gov/restles1.html

I suspect that CO-OPS knows more about tides than either Britannica or
Encarta.



"Down antenna"

>> Issac Newton originally explained the tides, but it appears the
>> writers and ediors of Encarta didn't bother to check on good old
[quoted text clipped - 33 lines]
> Sooooo
> It's back to the library.
Michael Mcneil - 10 Feb 2005 07:22 GMT
> "Up antenna!"

> Mike! I don't mean to flame you. But, in the below discussion you mention
> that New Orleans might be a good place from which to compare tide
> generation.

I was being clever. I knew that New Orleans didn't fit either simple
descriptions. I didn't know it was an even better example. Thanks for
the input.

> FYI:  The tides in New Orleans are so controlled by the Mississippi River
> that NOAA (the Natioanl Oceanic and Atmospheric Administration, an agency
> within the U.S.Department of Commerce) does not have a tide gage at New
> Orleans. Nor do they publish predictions or actual water levels for N.O.
> The closest tide gage is many miles south of New Orleans at Southwest Pass
> in the Mississippi delta.

When in the future this all crops up again and I attempt to disabuse the
next generation of indoctrinated monkeys I will bear all this in mind.

No one here want to mention Fiji?

> New Orleans is on the Mississippi River not on the Gulf of Mexico.

I always thought the Mississippi rolled out into the Gulf. I am rather
lackadaisical in my research (relying on my ablity to know it all.)

> For a rather good explanation of tidal forces, go to:

> http://www.co-ops.nos.noaa.gov/restles1.html

> I suspect that CO-OPS knows more about tides than either Britannica or
> Encarta.

Got it bookmarked. But I suspect the reason is that tides in the region
are so small that compared to river spates due to rainfall etc., having
a prediction is pointless

It's horses for courses with encyclopaedae. The Encarta is geared for
schoolchildren and the home environment and as such aught to be
more dilligent in its presentation of facts as it is indoctrinating
young minds.

The Enc. Brit. should be on the ball too, as it is written by the
expert's experts.

The plain fact is even I make mistakes. (And sometimes I admit to them.)
Hatunen - 10 Feb 2005 16:42 GMT
>> New Orleans is on the Mississippi River not on the Gulf of Mexico.
>
>I always thought the Mississippi rolled out into the Gulf. I am rather
>lackadaisical in my research (relying on my ablity to know it all.)

By that reasoning Minneapolis is on the Gulf of Mexico.

   ************* DAVE HATUNEN (hatunen@cox.net) *************
   *       Tucson Arizona, out where the cacti grow         *
   * My typos & mispellings are intentional copyright traps *
Michael Mcneil - 11 Feb 2005 13:58 GMT


> >> New Orleans is on the Mississippi River not on the Gulf of Mexico.

> >I always thought the Mississippi rolled out into the Gulf. I am rather
> >lackadaisical in my research (relying on my ablity to know it all.)

Or rather by my schoolboy's atlas, the connurbation stretches over to
the Mississippi Sound.

The globe I usually reach for first is not detailed enough for me to
distinguish how far up the delta New Orleans really is.

Well I learned something. Who knows if I will ever find it more useful
than to belabour holders of deeply entrenched ideas with.

Or at least attempt to muddy the waters enough to get some grey matter
stirred.

NBL; I know.
Hatunen - 11 Feb 2005 22:05 GMT
Just for the record, none of this quotes me.

>> >> New Orleans is on the Mississippi River not on the Gulf of Mexico.
>
[quoted text clipped - 14 lines]
>
>NBL; I know.

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Michael Mcneil - 11 Feb 2005 22:15 GMT
Who said that?
Hatunen - 12 Feb 2005 17:58 GMT
>Who said that?

Who said what?

   ************* DAVE HATUNEN (hatunen@cox.net) *************
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Weatherlawyer - 14 Feb 2005 12:02 GMT
Michael Mcneil - 28 Aug 2005 22:26 GMT
NOW have I rather passed over than thoroughly surveied all Britaine,
namely those two most flourishing Kingdomes England and Scotland. And
whereas I am now to crosse the seas for Ireland and the rest of the
Isles, if I praemise some few lines touching the British sea, I hope it
shall not seeme a crooked course or an extravagant digression.

2. Britaine is incompassed round about with the vast and open maine
Ocean, which ebbeth and floweth so violently with maine tides that, as
Pytheas of Marsiles hath reported, it swelleth 80 cubits about Britaine,
and Saint Basile hath tearmed it

mare magnum &c., that is, The great Sea and dreadfull to Sailers,

Yea and Saint Ambrose wrote thus of it:

The great Sea not adventured on by sailers, nor attempted by mariners,
is that which with a roaring and surging current environeth Britaine,
and reacheth into farre remote parts and so hidden out of sight as that
the very fables have not yet come thither.

Certes, this sea sometimes overfloweth the fields adjoining, otherwhiles
again it retireth and leaveth all bare, and, that I may use the words of
Plinie,

by reason of this open largenesse it feeleth more effectually the force
and influence of the Moone, exercising her powre thereupon without
impeachment. And it floweth alwaies up within the land with such
violence that it doth not onely drive backe the streames of rivers, but
also either overtaketh and surpriseth beasts of the land, or else
leaveth behind it those of the sea.

For there have bin seene in every age, to the great astonishment of
the beholders, so many and so huge Sea-monsters left on drie land upon
our shore that Horace sang this note not without good cause:

> Who said that?

Noe aediea butteth yt ame onne ye ynternette soe ytte myst be anne
tuethe.

{Alle ofn eate}
Fizziwig2 - 28 Aug 2005 23:40 GMT
William Camden,
Britannia (1607)?

> NOW have I rather passed over than thoroughly surveied all Britaine,
> namely those two most flourishing Kingdomes England and Scotland. And
[quoted text clipped - 37 lines]
>
> {Alle ofn eate}
Weatherlawyer - 22 Sep 2005 21:32 GMT
> William Camden,
> Britannia (1607)?

Beg pardon for the late reply. I have been having too much fun trolling
and flaming and otherwhiles etceterra, president Bush and his handlers.

<Slap> Naughty Mike </slap>

I have lost the link. I may have it on my desktop or lost somewherre
yne ye bowles of my computer. Blowed if I can understand what makes
msn's desktop search work. (I aught to stick with the file search
engine in the start menu.) Sorry.

The point I was was making was the ancient reliance on the presumption
about the lunar theory of raisng tides predates most renaissance
thinking.

Consider (if you have the mathematical ability) how the genii (such as
Poncelet) at the turn of the 19th century might have applied calculus
and the duality of linear motion to the behaviour of gravitational
attractive forces on the chords the sun and moon produce, had there not
been a war on.

There is certainly no restriction on paper to the link between tides
and the recipocrity of quakes. From what little I understand of the
subject at least.

There may be restrictions of course. Giant ones no doubt; that I in my
ignorance can't even begin to grasp. But I live in the school of the
keep it really simple stupid, -for obvious reasons.
Michael Mcneil - 22 Sep 2005 23:32 GMT
> Consider (if you have the mathematical ability) how the genii (such as
> Poncelet) at the turn of the 19th century might have applied calculus
> and the duality of linear motion to the behaviour of gravitational
> attractive forces on the chords the sun and moon produce, had there not
> been a war on.

OOF!

There is a hell of a lot of stuff out there on this duality thing. I can
not locate what I am after but the idea works like this:

View the earth as a disk (the conic section in the theory I was thinking
of) and the tangents forming the chord are those of the line(s) of sight
of the moon (and sun.) The triangle formed as the tangents, produce a
chord that divides the earth into day or night.

(There is a tidal day as well as the normally accepted term. It is
commonly thought of as being 55 minutes longer than the normal one.
Obviously not true for a variety of astronomical reasons. But the
geometry is there.)

Anyway; draw a series of these chords as the "day" changes and join the
dots.

Can anyone on sci.maths make some sense of that for me, please?

And use small words an idiot can follow, I beg you?
George - 29 Aug 2005 03:25 GMT
<Big snip>

Umm, we've got a cat 5 hurricane going, Mick.  What?  No earthquake
predictions?
 
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