Outlines of a mechanical theory of storms : $b containing the true law of lunar influence, with practical instructions to the navigator, to enable him approximately to calculate the coming changes of the wind and weather, for any given day, and for any part of the oceanBassnett, Thomas
Science
Outlines of a mechanical theory of storms : $b containing the true law of lunar influence, with practical instructions to the navigator, to enable him approximately to calculate the coming changes of the wind and weather, for any given day, and for any part of the ocean
Bassnett, Thomas
Weather
Now, the ether comes down the axis with the temperature of space, and
may possibly derive a _little_ additional temperature in passing over
the body of the sun; so that in this position the earth is protected
from the chilling influence of the radial stream, by being protected by
the body of the sun. And although, from the immense velocity of the
ether, it cannot derive much additional temperature, there may still be
an appreciable difference, due to this cause.
It is the chilling influence of the ethereal stream which originated the
idea among philosophers, of _frigorific impressions, darted from a clear
sky_. In some years the sun will be nearly in the centre of the system;
in other years the axis of the vortex will not come near the sun. And as
the sun's longitude may vary through the entire circle, it may happen
that the earth's longitude shall coincide in winter or summer, or spring
or autumn. When, however, the earth emerges from the protection of the
sun, and enters the conical shell, considered as a space of considerable
depth, she will again be exposed to the full force of the radial stream,
rendered more active by the previous deflection, and by the numerous
cross currents pervading it; so that a mild and calm winter may be
succeeded by a cold and stormy spring. The present season, (1853) the
earth's longitude coincided with the sun's longitude in about 135°, and
consequently was in the conical space spoken of, during February and
March; but the radius vector of the sun's centre, being then less
than 300,000 miles, the protection was not as complete as it is
sometimes. Still, the general fineness of these months was remarkable;
yet in April and May, when the earth became again exposed to the action
of the solar stream, the effect was to retard the spring, and disappoint
the prognostications of the weather-wise. In applying these principles,
we must consider the effect in those latitudes which are more readily
affected,--that is, in the temperate zone, midway between the two
extreme zones of heat and cold.
In 1837 and 1838, the longitude of the sun's centre corresponded with
the earth's, in August and September, when there was neither rain nor
electrical excitement; and consequently those seasons were sickly over
the whole country. Now, there is another cause which renders the months
of August, September, and October, deficient in electrical energy, and
consequently more prone to be sickly. If, therefore, the two causes
unite their influence, the autumnal months will be more sickly at those
times. This last cause, however, only affects the _northern latitudes_
in autumn, and consequently, _ceteris paribus_, the autumnal months
should not be so proverbially sickly in the southern hemisphere. This
is, however, only suggestive.
Public-domain text, read in full here on John Shaqi.
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