In Track & Field, the effect of air assistance or resistance is
acknowledged strongly enough such that the air flow is measured during
or around a race, and if it is too strong, then a wind-aided time
cannot count as a record.
Also in Track & Field, I don't know if there was an adjustment of the
rules after the Mexico City Olympics in acknowledgement that, in some
events, the thin air may have helped accomplish world records that
were a bit more statistically "outliers" than was expected at that
time (Bob Beamon's Long Jump, the strong world records in the Men's
400 meters and 200 meters, etc.).
So, with these thoughts in mind, I started wondering if the outcome of
some events might be affected by the moderate ebb and flow of
gravitational forces, such as are related to the Moon and perhaps (to
a lesser extent) the sun or even localized to certain parts of the
globe. While the changes in forces may be comparatively minute, so
too are the fractions of seconds that determine world records and
winners and losers. Maybe an historical statistical study could be
easily done, looking at performance versus the tides or versus some
local empirical measurement of gravitational forces. Are such
measurements taken? Perhaps not. Well, we know something of the
tides, so I guess that could be a proxy.
jl
google "channel swimming"
Tom Davidson
Richmond, VA
Yes. After I posted my question I realized that I'd left out an
important part which is that any trend after the 1968 Olympics to
recognize that performing at altitude may have influenced the outcomes
of events is a trend that was taking into account both wind resistance
and gravity. Both are reduced at altitude, as is the amount of
available air for endurance event participants to breathe.
So, I was accustomed to thinking of the outfall of the '68 Olympics as
an air resistance thing, but I guess it would also be a recognition of
gravitational efffect upon performance?
I've been taught most of my life that the tides are, for the most
part, a result of the interaction of the moon with the Earth, so even
granting your equations, the effect of the Earth-moon interaction at
sea level seems to be palpable for bodies of water, and perhaps also
palpable for elite athletic competition. Now, it may not be a simple
matter of the Moon's pull so much as that plus some aspects of the
Earth's rotation and orbit that are harder to understand?
jl
The larger, and measureable effects are from the air, and 99% will be the
skill and attitude of the athlete.
More dense air in cold pressure areas, and at sea level will affect
performance two ways.
You get more oxygen, but have more air to push through.
At higher altitudes and lower pressure, that is reversed in still air.
Moving air adds its own force.
Don't blame the air, unless you're willing to stop using it.
"David Williams" <david.w...@bayman.org> wrote in message
news:1219113535.8...@bayman.org...
Yes, even at 3 miles altitude, it is *possible* to breathe, and with
conditioning, even live. People in Chile have developed their bodies in
these conditions.
Astronomers regularly have observatories at these altitudes.
Above that, and especially on Everest, where more than a third of the people
die in the attempt, oxygen is carried in tanks.
Athletics in those conditions is dangerous.
"David Williams" <david.w...@bayman.org> wrote in message
news:1219189335.8...@bayman.org...
'Wiki' has an article that I skimmed, and shows a difference in wieght of
.28% with over 8000 m in height. I doubt any measurable difference in an
athletes performance could be measured that finely.
http://en.wikipedia.org/wiki/Earth's_gravity
"David Williams" <david.w...@bayman.org> wrote in message
news:1219246633.8...@bayman.org...
"BBO" <az...@dod.no> wrote in message
news:n6SdndEitLT...@telenor.com...
> Ralph wrote:
>> Use some figures that make sense. Your answer is a small percentage of
>> your error in estimation. The earths mass is grossly estimated at 5.97 x
>> 10^24 kg, (note the error in the 10^21 kg range) and the diameter,
>> depending on how you take it, about 7926 miles. (error in miles) How do
>> you justify an answer in mm. or the weight of an athlete or his
>> equipment?
>
> Given a spherical cow of uniform density we easily see that....
>
> Read: In theory and working with exact numbers you can justify those kind
> of numbers. In reality - not possible, because we all know there is no
> such cow.
>
> --
> You can't be a rational person six days a week...and on one day of the
> week, go to a building, and think you're drinking the blood of a two
> thousand year old space god. -- Bill Maher
Your guesses at numbers with errors on the order of (corrected) kilometers,
with answers in millimeters, are the nonsense here.
Math can't be accurate unless the answer is greater than (you don't seem to
comprehend this) the error in the original numbers.
Since your answer is orders of magnitude LESS than your errors in guessed-at
figures, your original statements and math are invalid.
The math from Wiki gives estimates for a model of gravity for a planet with
ideal condition of even density, and all other factors the same. It's
stated in the article.
In that *theoretical* world, using your estimates, a .1% difference would
change the weight of a 100 kg. athete by 100 grams.
Had a sandwich lately? It weighs more.
Realistically, that's neglible. All the other factors, including the mood
of the athlete, the weather that day, and lots more I'm sure an actual
athlete could name better than I, would be more notable than any change in
gravity.
That's why gravity is such a hot topic in physics. It's only recently that
equipment has been designed to work on such small differences. -on the
order of 10^-20 g.
Go for any numbers you make up and believe. I'll stick with the measured
results.
Have fun.
"David Williams" <david.w...@bayman.org> wrote in message
news:1219592763.8...@bayman.org...
Your denial of math logic, and the concept of gravity without using the most
basic part of it, are flawed.
The insignifcant values that you plug into your imaginary formulations give
you numbers that you're welcome to believe, done in your head, and
therefore, imagined true. If that's what you believe, you're welcome to
believe that an athletes mass is more important to gravity than the mass of
the earth.
This is a fairly simple concept, even in Newtonian gravity.
Result error based on inaccurate input is also fairly basic.
Keeping it simple: Garbage in, garbage out.
Your guesstimates seem to be increasing with your posts, so there's no
consistancy there.
This seems to be a philosophical tirade, since there are so many other
factors, and all other things would not be equal.
What I'm saying is that gravity is neither a measureable effect, or even one
that needs consideration in athletics.
I will never deny that athletic records are meaningless, so don't go putting
more words in my honour.
Actually, go ahead. It's fun to read and pass along to friends.
I'll say, not what you're trying to goad me into, but what I've backed up.
Simple, stupid.
"David Williams" <david.w...@bayman.org> wrote in message
news:1219679784.8...@bayman.org...
So is that why high jumpers and pole-vaulters do
better when the moon is full, because of tidal force?
Ken
PS:Usually Daves "guestimates" are as accurate
as my calculator!
"all other things being equal" is a partial derivative.
"Ken S. Tucker" <dyna...@vianet.on.ca> wrote in message
news:2ba8f80c-ac3c-4626...@z6g2000pre.googlegroups.com...
On Aug 25, 3:33 pm, "Ralph" <aj...@ncf.ca> wrote:
> Very good.
> Go to the head of the class!
Thanks:-). Your discussion got to me to thinking
if we launched a rocket (all other things being equal)
at high tide (full or new moon) if less propellant
would be required to achieve the same orbit if we
launched at neap tide.
I'm hoping for a simple answer, otherwise I'll need to
enter the Riemann Christoffel "tidal tensor", R_abcd
into the geodesic.
Regards
Ken
> "Ken S. Tucker" <dynam...@vianet.on.ca> wrote in messagenews:2ba8f80c-ac3c-4626...@z6g2000pre.googlegroups.com...
On Aug 25, 5:09 pm, david.willi...@bayman.org (David Williams) wrote:
> You're revealing yourself as an idiot.
>
> If you think that calculations done as you think they should be done
> will produce a conclusion different from mine, then let's see them. Put
> up, or shut up.
>
> I don't include the earth's mass in my calculation because I can see in
> advance it will cancel out. In order to calculate a jumper's takeoff
> velocity, I will have to start with the distance he can jump, since
> that's a measured quantity, and work backward, using the earth's mass.
> Then I'll work forward again, using the mass again, and it will simply
> cancel out! So I might as well just use the distance a jumper can
> jump in the calculation, and not worry about the earth's mass.
While I lurked this discussion, I was replaying
(in my mind) the video of the Apollo astronauts
on the moon, but that could be a "red herring".
> Ken Tucker has known me for decades.
Dave, you are too complex to really know,
but I'll try for a few more decades ;-).
> If he criticizes my logic, I take the criticism seriously.
LOL, you never did before, but really, the equation is
acceleration = GM/r, with a minor variance on "r",
should I Rubber Bible G,M,r and dr ?
> dow
Regards
Ken
I was descending to a level of name-calling I didn't like, (but the source
shows) and no amount of logic can change that. (or any fantasy)
I'll leave cancelling the earths gravity to the source that brought it into
the subject.
Maybe I'll go watch a tide.
Thanks again,
"Ken S. Tucker" <dyna...@vianet.on.ca> wrote in message
news:e0c4418d-c9d0-41da...@t1g2000pra.googlegroups.com...
On Aug 26, 6:46 am, "Ralph" <aj...@ncf.ca> wrote:
> Thanks Ken,
> I was descending to a level of name-calling I didn't like, (but the source
> shows) and no amount of logic can change that. (or any fantasy)
It may not be a direct extrapolation of radius,
perhaps local density has an effect.
> I'll leave cancelling the earths gravity to the source that brought it into
> the subject.
> Maybe I'll go watch a tide.
Check out "sci.physics.foundations" , it's moderated.
Regards
Ken
That's sweet the way it works out.
> So if r2/r1 = 1.0005, which will be true if r1 = 6000 and r2 = 6003 (in
> kilometres), then d2/d1 qill be 1.0005^2, which is almost precisely
> 1.001. If d1 = 6 (metres), d2 will be 6.006 metres. In other words, at
> an altitude of 3000 metres, a good long-jumper who can jump 6 metres at
> sea level will be able to jump 6 millimetres further. Since distances
> are measure to the nearest centimetre, his jump distance will probably
> be counted as 1 cm further than at sea level.
I think that same distance would ratio in Pole-Vault
as well (?). We can turn that (1.001) around to a
reduction of 1gm / Kg of the jumpers weight, so
an 80Kg athelete would jump 1/cm further for each
80 gms of weight loss.
The reason I'm curious is because (IIRC) the womens
long jump was 1 cm different, between 1st and 2nd.
If 80 gm's is true we're looking at shoe, bra and tampax
weight, and maybe even pooping before the jump :-).
> Ken, I'm sure this was obvious to you.
It's obvious now! 1 part in 1000 outputs 1 cm yeah(?).
Regards
Ken
>-> Thanks. I'll concentrate on the altitude and its effect on weight and
> -> the effect this might have on sports performance.
>
> Well, in an extreme case, altitude might alter the weight (but not the
> mass) of an athlete by about 0.1 percent.
Actually, latitude is the more important determinant of local gravity as
experienced in practice (that is net of centrifugal force) on Earth.
Plugging values into the relevant formula, I see that to obtain local
gravity as low as experienced at sea level at the equator, I would have
to ascend a mountain of 10,700m at my own latitude of 53 degrees. Of
course, no such mountain exists.
At 60 degrees 35' north, net gravity is 0.4% greater than at the
equator, so it's realistic to account for differences of 0.4% in local
gravity between athletic stadia.
So suppose in the long-jump
> the distance a jumper can go is inversely proportional to the force of
> gravity pulling him down,
Given equal initial vertical velocity, the time in the air is inversely
proportional to the _square root_ of the local gravity (this is related
to the units of local gravity being length divided by time _squared_).
So, with 0.1% lower gravity and take off speed being equal, you could
expect approximately 0.05% increase in distance; with 0.4% lower
gravity, approximately 0.2% increase.
then if he can jump about 5 metres, he might
> go 5 millimetres further at high altitude than at sea level, from this
> cause.
My upper end value of 0.2% would yield a 16mm increase to an 8m jump (a
jump at the lower end of male international standard). Horizontal jumps
are measured to the nearest 1cm, so this would be above the official
threshold of significance.
More striking, perhaps, the difference to a world record men's triple
jump (somewhat over 18m), would be 5cm or 6cm as measured. This is not
just theoretical, as Jonathan Edward's 1995 world record of 18.29m was
set in Goteborg in Sweden, a seaport 57.7 degrees North, so this may be
equivalent to 18.34m at the equator.
Also, there would be less air resistance slowing him down, so he
> should be able to jump further still.
I can confirm your assessment of the importance of air resistance, David
- it is generally recognised as being a major factor in athletic
performance. When decreased air resistance is due to following winds it
is officially recognised, and world records cannot be set in certain
track and field events unless there is a record of the wind speed and it
doesn't exceed 2 m/s in the direction of motion. I think empirical
analysis shows that wind assistance of 2 m/s is worth about 0.1s in a
world class men's 100m (so about 1%) - in any event, it can contribute
substantially more than gravity differences.
Since the 1968 Mexico City Olympics, there have often been debates in
athletics circles about whether similar status should be given to
performances that are "altitude assisted", because of the lesser air
resistance. Indeed, there was a time when some people kept unofficial
low-altitude world records for (principally) the men's 100m and men's
long jump, because the records set in 1968 at over 2000m altitude were
not being seriously challenged.
Beamon's long jump record was the most celebrated of these records, and
it had been set with the maximum allowable 2 m/s wind assistance as
well. Using a standard formula for fluid drag resistance, and assuming
air density at 75% of sea-level and that Beamon travelled at 10 m/s, I
calculated the combined reduced air resistance as equivalent to 3.5 m/s
wind assistance at sea level. So, there are strong grounds for arguing
that Beamon's performance had more environmental assistance than other
performances that were ineligible for accreditation as world records.
Beamon's record was broken in 1991, and afterwards the debate died down
about officially recognising "altitude assistance" for performances. As
to gravity differences affecting performances, I've never been aware of
it being debated in athletic circles.
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Much less math is needed if you check the facts.
"Peter Munn" <pmun...@pearce-neptune.demon.co.uk> wrote in message
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