MAGNETIC STORMS.

The mysterious course of the magnetic needle is equally affected by

time and space, by the sun’s course, and by changes of place on the

earth’s surface. Between the tropics the hour of the day may be known

by the direction of the needle as well as by the oscillations of the

barometer. It is affected instantly, but transiently, by the northern

light.

When the uniform horary motion of the needle is disturbed by a magnetic

storm, the perturbation manifests itself _simultaneously_, in the

strictest sense of the word, over hundreds and thousands of miles of

sea and land, or propagates itself by degrees in short intervals every

where over the earth’s surface.

Among numerous examples of perturbations occurring simultaneously and

extending over wide portions of the earth’s surface, one of the most

remarkable is that of September 25th, 1841, which was observed at

Toronto in Canada, at the Cape of Good Hope, at Prague, and partially

in Van Diemen’s Land. Sabine adds, “The English Sunday, on which it is

deemed sinful, after midnight on Saturday, to register an observation,

and to follow out the great phenomena of creation in their perfect

development, interrupted the observation in Van Diemen’s Land, where,

in consequence of the difference of the longitude, the magnetic storm

fell on Sunday.”

It is but justice to add, that to the direct instrumentality of the

British Association we are indebted for this system of observation,

which would not have been possible without some such machinery

for concerted action. It being known that the magnetic needle is

subject to oscillations, the nature, the periods, and the laws

of which were unascertained, under the direction of a committee

of the Association _magnetic observatories_ were established in

various places for investigating these strange disturbances. As

might have been anticipated, regularly recurring perturbations were

noted, depending on the hour of the day and the season of the year.

Magnetic storms were observed to sweep simultaneously over the

whole face of the earth, and these too have now been ascertained to

follow certain periodic laws.

But the most startling result of the combined magnetic observations

is the discovery of marked perturbations recurring at intervals of

ten years; a period which seemed to have no analogy to any thing

in the universe, but which M. Schwabe has found to correspond

with the variation of the spots on the sun, both attaining their

maximum and minimum developments at the same time. Here, for the

present, the discovery stops; but that which is now an unexplained

coincidence may hereafter supply the key to the nature and source

of Terrestrial Magnetism: or, as Dr. Lloyd observes, this system of

magnetic observation has gone beyond our globe, and opened a new

range for inquiry, by showing us that this wondrous agent has power

in other parts of the solar system.

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