The Philosophy of the Weather. And a Guide to Its ChangesButler, T. B. (Thomas Belden)
Science
The Philosophy of the Weather. And a Guide to Its Changes
Butler, T. B. (Thomas Belden)
Weather; Weather forecasting
"The whole experiment serves to demonstrate that such an active
gyration as we have ascribed to storms, and have proved, as we deem,
to appertain to some, at least, of the more violent class; must
necessarily expand and spread out, _by its centrifugal action, the
stratum of atmosphere subject to its influence, and which must,
consequently, become flattened or depressed by this lateral movement,
particularly toward the vortex or center of the storm_; lessening
thereby the weight of the incumbent fluid, and producing a consequent
fall of the mercury in the barometrical tube. This effect must
increase, till the gravity of the circumjacent atmosphere, superadded
to that of the storm itself, shall, by its counteracting effect, have
produced an equilibrium in the two forces. Should there be no
overlaying current in the higher regions, moving in a direction
different from that which contains the storm, the rotative effect
may, perhaps, be extended into the region of perpetual congelation,
till the medium becomes too rare to receive its influence. But
whatever may be the limit of this gyration, its effect must be to
_depress_ the _cold stratum_ of the upper atmosphere, particularly
toward the more central portions of the storm; and, by thus bringing
it in contact with the humid stratum of the surface, to produce a
permanent and continuous stratum of clouds, together with a copious
supply of rain, or a deposition of congelated vapor, according to the
state of the temperature prevailing in the lower region."
The italics in the foregoing extract are mine; and, in relation to it, I
observe:
1st. There is no cylindrical vessel around storms, and _air will not thus
resist air_. Confessedly, such resistance is necessary. Let any one watch
his cigar smoke, and see how readily it moves on, with little momentum.
Let any one try the experiment of creating a whirl in the _open air_, or
in a room, or box of paper, or other material, which can be suddenly
removed, with air colored by smoke. I am exceedingly mistaken if he does
not find the presence of a "cylindrical vessel," absolutely essential to
prevent the instantaneous tangential escape of the air.
2d. Turn back to page 3 and look at the fall of the barometer in the polar
regions (recorded in the extract from Dr. Kane), with _scarcely any
wind_, and _as little variation_ in its _direction_, and see how utterly
Mr. Redfield's theory fails to account for the phenomena.
3d. If I understand Mr. Redfield correctly, he has abandoned the claim as
originally made, that the wind moves in circles, expanding, and _spreading
out_ by a "_lateral movement_," and now asserts that it blows spirally
inward, and elevates the air in the center. I quote:
Public-domain text, read in full here on John Shaqi.
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