ROUTINE OF A STORM.

The novelty and originality of this theory will perhaps justify us in

dwelling a little longer on what observation has detected. The vortex

(and we are now speaking only of the central vortex) does not derange

every place alike, but _skips_ over large tracts of longitude in its

progress westward. We speak here of the immovable axis of the vortex as

in motion; in reality it is the rotation of the earth which brings every

meridian under its influence in some latitude once every twenty-four

hours. The centre of greatest derangement forms the nucleus, towards

which the surface currents, under certain restrictions, flow. The

strongest current will, however, usually be from the south, on account

of the inclination of the axis of the vortex to the surface of the

earth.[8] These currents continuing onwards by their vires inertiae,

according to the first law of motion, assist somewhat in conveying the

warm surface wind, loaded with moisture, into the region of cloud; and

the diminution of temperature causes the condensation of large masses of

vapor, according to Hutton's views; and the partial vacuum thus

produced, causes a still greater intermingling. But we have already

shown that this is not the sole cause, nor is it ever more than

partially accomplished. The ether of the lower atmosphere, and of the

crust of the earth, is disturbed, and rushes towards the rarefied axis

from the surface, and with the temperature of the surface, thus

conveying the surface atmosphere, in a measure, along with it. In the

upper regions, this ether (or electric fluid) cools down, or parts with

some of its heat, to the air of those regions, and, by its great

specific caloric, necessarily and unduly increases the temperature of

the air. This, by its expansion and ascension will cause a further

influx from below, until the upper atmosphere becomes loaded with vapor.

In twelve hours, at least, a reaction must take place, as that part of

the earth's surface is carried six or seven thousand miles from the

axis, where the ether is more dense. This in turn descends to the

surface, carrying with it the temperature of space, at least 60d below

zero; a great condensation must follow; local derangements of the

electric equilibrium in the centre of large clouds, when the

condensation is active, must now take place, while partially

nonconducting masses intervene, to prevent an instantaneous restoration

of the equilibrium, until the derangement is sufficient to cause the

necessary tension, when all obstacles are rent asunder, and the ether

issues forth, clothed in the power and sublimity of the lightning. It is

a fearfully-energetic fluid, and, when sufficiently disturbed, competent

to produce the most violent tornado, or the most destructive earthquake.

That these two phenomena have simultaneously occurred, seems well

authenticated; but the earthquake, of course, must be referred generally

to derangements of the electric equilibrium of the earth's interior, of

which at present we know but little.

The day or morning previous to the passage of the vortex, is frequently

very fine, calm, mild, and sleepy weather,--commonly called a weather

breeder. After the storm has fully matured, there is an approach of the

clouds to the surface, a reduction of the temperature above, and the

human body feels the change far more than is due to the fall of

temperature. This is owing to the cold ether requiring so much heat to

raise its temperature to that of surrounding bodies, or, in other words,

is due to its great specific caloric. In summer, this falling of the

upper layers in front of the storm is so apparent, that every part is

seen to expand under the eye by perspective,--swelling, and curling, and

writhing, like the surface of water or oil when just commenced boiling.

The wind now partakes of the motion of the external ether, and moves

with the storm eastward (in this latitude), or from N-E. to S-E., until

the action ceases.

Outlines of a mechanical theory of storms · 第 48 / 118 题