Astronomy in a nutshell : $b The chief facts and principles explained in popular language for the general reader and for schoolsServiss, Garrett Putman
Science
Astronomy in a nutshell : $b The chief facts and principles explained in popular language for the general reader and for schools
Serviss, Garrett Putman
Astronomy -- Juvenile literature
Besides the horizon and the zenith there is one other thing of
fundamental importance which we must learn about before proceeding
further,—the meridian. The meridian is an imaginary line, or semicircle,
beginning at the north point on the horizon, running up through the
zenith, and then curving down to the south point. It thus divides the
visible sky into two exactly equal halves, an eastern and a western
half. In the ordinary affairs of life we usually think only of that part
of the meridian which extends from the zenith to the south point on the
horizon (which is sometimes called the "noon-line” because the sun
crosses it at noon), but in astronomy the northern half of the meridian
is as important as the southern.
=4. Altitude and Azimuth.= Now, suppose that we wish to indicate the
location of a star, or other object, in the sky. To do so, we must have
some fixed basis of reference, and such a basis is furnished by the
horizon and the zenith. If we tried to describe the position of a star,
the most natural thing would be, first, to estimate, or measure, its
height above the horizon, and, second, to indicate the direction in
which it was situated with regard to the points of the compass. These
two measures, if they were accurately made, would enable another person
to find the star in the sky. And this is precisely what is done in
astronomy. The height above the horizon is called altitude, and the
bearing with reference to the points of the compass is called azimuth.
Together these are known as co-ordinates. In order to systematise this
method of measuring the location of a star, the astronomer uses
imaginary circles drawn on the celestial sphere. The horizon and the
meridian are two of these circles. In addition to these, other imaginary
circles are drawn parallel to the horizon and becoming smaller and
smaller until the uppermost one may run close round the zenith, which is
the common centre of the entire set. These are called altitude circles,
because each one throughout its whole extent is at an unvarying height,
or altitude, above the horizon. Such circles may be drawn anywhere we
please, so as to pass through any chosen star or stars. If two stars in
different quarters of the sky are found to lie on the same circle, then
we know that both have the same altitude.
[Illustration:
_Fig. 2. Altitude and Azimuth._
Public-domain text, read in full here on John Shaqi.
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