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
This excess of magnetic intensity and electricity not only gives a
peculiar character to our vegetation, but also to our race, our animals,
and every thing. He who supposes that the restless activity and energy of
the people of the United States is the result of habit, or education, or
any fortuitous circumstances alone, is mistaken. Let him watch the
contrast in his own feelings during those occasional languid, damp, and
sultry, although not thermometrically, hot days--which so much resemble
the summer weather of England--with those days of bright, bracing, N. W.
and S. W. air, so much more frequent here, and he will appreciate the
difference. That term "bracing," so much in use, will express the effect
of this peculiar weather. It "girds up the loins," both of body and mind.
Men and animals can work with more ease, even in our peculiar extremes of
heat, than they can in England, and fatten with less.
A similar difference in degree is found between our climate and that of
the Pacific portion of our country. Something is due to the difference in
the volume and moisture of the counter-trades, and something to the
contiguity of the Pacific Ocean; but to the difference in
magneto-electric intensity, the contrast is mainly due. Corn and cotton
will be grown, to some extent, in the valleys west of the meridian of
105 deg., but never as successfully as east of it.
The aurora is periodical, like all the other atmospheric phenomena, but
its periodicity is not accurately ascertained. It is believed to have
occurred much oftener during the second quarter of this century, than
during the first. It is known, however, to occur most frequently in the
spring and fall; and during those periods when the active and rapid
transit of the atmospheric machinery produces the greatest degree of
magnetic disturbance. This identifies it with terrestrial magnetism.
Dalton gives us the following table of observations, arranged according to
the months when they were seen.
Jan. Feb. Mar. Apr. May. June. July. Aug. Sept. Oct. Nov. Dec.
(1) 18 18 26 32 21 5 2 21 23 36 38 9
(2) 21 18 23 13 3 2 1 3 35 22 22 21
(3) 21 27 22 12 1 5 7 9 34 50 26 15
(4) 5 6 4 8 10 7 6 14 14 17 5 6
(1) contains those observed by him at Kendall; (2) are taken from another
list; (3) is MARIAN'S list of those observed before 1732; and (4), those
seen in the State of New York in 1828 and 1830.
Mr. Stevenson's table of those observed by him at Dunse, from 1838 to
1847, inclusive, is as follows:
Jan. Feb. Mar. Apr. May. June. July. Aug. Sept. Oct. Nov. Dec.
32 20 18 18 3 0 2 14 43 34 30 23
Public-domain text, read in full here on John Shaqi.
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