Aërial Navigation: A Popular Treatise on the Growth of Air Craft and on Aëronautical MeteorologyZahm, Albert Francis
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Aërial Navigation: A Popular Treatise on the Growth of Air Craft and on Aëronautical Meteorology
Zahm, Albert Francis
Aeronautics; Meteorology
The true horizontal speed anywhere in a tornado is compounded of the
velocities of gyration and of translation, as in the cyclone. Hence the
advancing side may be considerably the swifter and more destructive,
particularly more destructive since the impact of air increases as
the square of the velocity. If the vortex were stationary it would
be equally dangerous on all sides, standing erect and symmetrical;
but it drifts with the whole mass of air, sometimes quite swiftly and
often with varying speed of travel at different levels; thus, in its
slenderest forms, appearing bent and not infrequently twisted, as
it advances writhing serpentlike through the sky. Furthermore, the
intensity of whirl may fluctuate momentarily, with consequent shifting
of the isobaric surface, including that one whose form is visible
by reason of incipient condensation; and thus the funnel-like misty
tongue appears to dart earthward as a foggy downshoot from the cloud
above, whereas its parts are really rushing upward at all times very
swiftly, whether visible or not. This agile protrusion of the nimbus,
now a tongue, now a dark and mighty tower, is the strenuous part of
the storm, the abominated “twister” which the Kansan farmer sedulously
shuns, or peeps at from a hole in the ground. Unwelcome, indeed, are
its visitations, when, with mickle and multitudinous roar, it claps
his house in sudden darkness, hurls it aloft and sows its sacred relics
over all the adjoining township, “that with the hurly-burly hell itself
awakes.”
Theory, as well as experience, accredits the tornado with vast energy
and power. For, suppose a surface stratum of air one mile in area
and one thousand feet thick to increase in absolute temperature one
per cent, thus uplifting the superincumbent atmosphere ten feet. The
total energy stored in this way equals the weight lifted multiplied by
its upward displacement. The weight is a ton per square foot and the
displacement is ten feet; hence the stored energy is ten-foot tons per
square foot of the heated tract, or about 280,000,000 foot tons for
the square mile of heated air. This is equivalent to the work of one
million horses for over a quarter of an hour. A goodly percentage of
this stored work may be converted into kinetic energy in the active
part of the dry tornado. It is the energy of a vast reservoir suddenly
gushing through a tall penstock. It is a colossal upward cataract, an
aërial Niagara, a Johnstown flood suddenly liberated and quickly spent.
Public-domain text, read in full here on John Shaqi.
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