Meteorology: The Science of the AtmosphereTalman, Charles Fitzhugh
Science
Meteorology: The Science of the Atmosphere
Talman, Charles Fitzhugh
Meteorology
The late war gave prominence to certain acoustic phenomena which,
though hardly mysterious, were novel to the world at large. One of
those was the double report (triple in the case of an exploding shell)
heard near the line of fire of large guns. This effect is due to the
fact that modern projectiles travel much faster than sound. The moving
projectile sets up its own waves in the air, like those at the bow
of a steamer, which may reach the ear of the observer and produce the
sensation of a sharp sound before he hears the sound coming from the
mouth of the gun. Another phenomenon frequently observed when heavy
firing was in progress was the appearance in the sky of rapidly moving
parallel arcs of light and shade. These were generally seen against
clouds, but sometimes they swept across blue sky. They probably
occurred only in calm weather. These arcs were the result of the
successive condensations and rarefactions of the air constituting waves
of sound--visible sound waves. Their visibility was due to contrasts in
the refraction of light passing through air of different densities; the
same sort of refraction contrasts that cause the tremulous appearance
of the air over a hot stove, for example. The same “flashing arcs” of
light have been described by Prof. F. A. Perret as attending explosive
volcanic outbursts at the craters of Vesuvius and Ætna.
The humming of telegraph wires has been the subject of a certain
amount of discussion in meteorological circles, but without altogether
satisfactory results. This sound is not, of course, caused or affected
by the electric currents passing along the wire, and it is almost
certainly due solely to the wind, though the suggestion has been
made that it might be caused by the microseisms, or small and rapid
earthquake tremors, that are so commonly registered by seismographs
while imperceptible to the human senses. The humming is best heard
when one’s ear is placed against a telegraph pole. Several persons
have made systematic observations of these sounds from day to day,
and it has often been alleged that they vary with the temperature,
the movements of storms, etc., and even constitute a safe basis for
weather predictions. They are sometimes heard when the air appears to
be perfectly calm, but in such cases there might be some movement of
the air at the level of the wires, though there was none at the lower
level of the observer. From what is known about “æolian tones” (such
as those of the æolian harp), it would seem that the humming requires
a wind more or less at right angles to the wire, and that the pitch of
the sound depends upon the force of the wind and the diameter (but not
the length or tension) of the wire. For a given wire, the stronger the
wind the higher the pitch of its sound.
Public-domain text, read in full here on John Shaqi.
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