Appletons' Popular Science Monthly, December 1898: Volume LIV, No. 2, December 1898Various
Science
Appletons' Popular Science Monthly, December 1898: Volume LIV, No. 2, December 1898
Various
Science -- Periodicals; Technology -- Periodicals
Again, everybody knows that winter and summer, and the other
phenomena which simulate or accompany them, such as wet and
dry seasons, depend upon the fact that the earth's axis is not
perpendicular to the plane in which the earth moves round the sun,
but slightly inclined to it. Now, a year in itself, viewed as a
measure of time, is merely the period which it takes the earth to
perform one such complete revolution. During one half of each such
revolution the north pole is turned at a considerable angle toward
the sun, and during the other half, the south pole. When the north
pole is so turned we call it summer in the northern hemisphere;
when the south pole is being favored, and the north is receiving
less light and heat, we call it winter. Let us suppose for a moment
that the earth had not got this twist or kink in its axis; that
the equator was always presented exactly toward the sun; what then
would happen? Obviously, there would be no change of seasons. The
day and night would have fixed lengths which never varied; climate
would in each place be uniform and, barring accidents of elevation
or distribution of land and water, the climate of each place would
also depend entirely the whole year round on its distance from the
equator. Roughly speaking, the temperature of a district would be
the temperature it now possesses in March and September, only not
quite so cold as March nor so warm as September, owing to the absence
of accumulated heat from summer or of reserves of ice and snow from
winter. In one word, under such conditions there would have been
climates--marked belts of climate; but there would not have been
seasons.
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