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
While we retain the same place on the earth, the diurnal revolution
occasions no change in our horizon, but our horizon goes round, as well
as ourselves. Let us first take our station on the equator, at sunrise;
our horizon now passes through both the poles and through the sun, which
we are to conceive of as at a great distance from the earth, and
therefore as cut, not by the terrestrial, but by the celestial, horizon.
As the earth turns, the horizon dips more and more below the sun, at the
rate of fifteen degrees for every hour; and, as in the case of the polar
star, the sun appears to rise at the same rate. In six hours, therefore,
it is depressed ninety degrees below the sun, bringing us directly under
the sun, which, for our present purpose, we may consider as having all
the while maintained the same fixed position in space. The earth
continues to turn, and in six hours more, it completely reverses the
position of our horizon, so that the western part of the horizon, which
at sunrise was diametrically opposite to the sun, now cuts the sun, and
soon afterwards it rises above the level of the sun, and the sun sets.
During the next twelve hours, the sun continues on the invisible side of
the sphere, until the horizon returns to the position from which it set
out, and a new day begins.
Let us next contemplate the similar phenomena at the _poles_. Here the
horizon, coinciding, as it does, with the equator, would cut the sun
through its centre and the sun would appear to revolve along the surface
of the sea, one half above and the other half below the horizon. This
supposes the sun in its annual revolution to be at one of the equinoxes.
When the sun is north of the equator, it revolves continually round in a
circle, which, during a single revolution, appears parallel to the
equator, and it is constantly day; and when the sun is south of the
equator, it is, for the same reason, continual night.
When we have gained a clear idea of the appearances of the diurnal
revolutions, as exhibited to a spectator at the equator and at the pole,
that is, in a right and in a parallel sphere, there will be little
difficulty in imagining how they must be in the intermediate latitudes,
which have an oblique sphere.
Public-domain text, read in full here on John Shaqi.
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