Letters on Astronomy: in which the Elements of the Science are Familiarly Explained in Connection with Biographical Sketches of the Most Eminent AstronomersOlmsted, Denison
Science
Letters on Astronomy: in which the Elements of the Science are Familiarly Explained in Connection with Biographical Sketches of the Most Eminent Astronomers
Olmsted, Denison
Astronomy
I will next endeavor to explain to you the phenomena of the _Seasons_.
These depend on two causes; first, the inclination of the earth's axis
to the plane of its orbit; and, secondly, to the circumstance, that the
axis always remains parallel to itself. Imagine to yourself a candle
placed in the centre of a ring, to represent the sun in the centre of
the earth's orbit, and an apple with a knittingneedle running through it
in the direction of the stem. Run a knife around the central part of the
apple, to mark the situation of the equator. The circumference of the
ring represents the earth's orbit in the plane of the ecliptic. Place
the apple so that the equator shall coincide with the wire; then the
axis will lie directly across the plane of the ecliptic; that is, at
right angles to it. Let the apple be carried quite round the ring,
constantly preserving the axis parallel to itself, and the equator all
the while coinciding with the wire that represents the orbit. Now, since
the sun enlightens half the globe at once, so the candle, which here
represents the sun, will shine on the half of the apple that is turned
towards it; and the circle which divides the enlightened from the
unenlightened side of the apple, called the _terminator_, will pass
through both the poles. If the apple be turned slowly round on its axis,
the terminator will successively pass over all places on the earth,
giving the appearance of sunrise to places at which it arrives, and of
sunset to places from which it departs. If, therefore, the equator had
coincided with the ecliptic, as would have been the case, had the
earth's axis been perpendicular to the plane of its orbit, the diurnal
motion of the sun would always have been in the equator, and the days
and nights would have been equal all over the globe. To the inhabitants
of the equatorial parts of the earth, the sun would always have appeared
to move in the prime vertical, rising directly in the east, passing
through the zenith at noon, and setting in the west. In the polar
regions, the sun would always have appeared to revolve in the horizon;
while, at any place between the equator and the pole, the course of the
sun would have been oblique to the horizon, but always oblique in the
same degree. There would have been nothing of those agreeable
vicissitudes of the seasons which we now enjoy; but some regions of the
earth would have been crowned with perpetual spring, others would have
been scorched with the unremitting fervor of a vertical sun, while
extensive regions towards either pole would have been consigned to
everlasting frost and sterility.
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