Conja, Jerry & Steve:

I wept in envy for how fracking smart you all are, then my head exploded, but 
not before I laughed at the last statement.
Conja sees a multi-variable equation, I see a bumper-sticker; we all have our 
talents :oD

Leigh

On Feb 10, 2010, at 10:21 PM, Steve Haflich wrote:

> Conja Summerlin <[email protected]> wrote:
> 
>   On Wed, Feb 10, 2010 at 20:52, Jerry Houston <[email protected]> 
> wrote:
> 
>       Not to mention the loss of heat due to evaporation of your moist breath,
>       the rate of which would depend on the relative humidity of the air in
>       the horn ...
> 
> I would expect once the horn has been played a little I would expect the
> air in most of the horn's length to have similar humidity to breath
> exhaust.
> 
>   Let's not forget relative barometric pressure.
> 
> No, let's forget relative barometric pressure.  The pressure of a gas
> makes no difference to the speed of sound in that gas.  The
> _composition_ and temperature of the gas is what makes the difference
> (including slight effects of relative humidity) but the absence of
> effect due to pressure is what makes it possible to play the same horn
> at sea level and in elevated cities such as Denver.
> 
> In Denver, if you were playing outdoors, the adiabatic temperature would
> make the temperature about 10 degrees C colder than the temperature at
> sea level, and this would make a difference.  This is why most concert
> halls have central heating, especially in Denver.
> 
> At extreme altitudes (e.g. the stratosphere) the speed of sound changes
> because the composition of atmosphere changes with altitude.  But the
> composition is relatively constant throughout altitudes where it is
> possible to play.
> 
> ==========
> 
> In a vacuum no one can hear you clam.
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