The time a planet requires to make one circuit of its orbit
constitutes, as with the earth, its year. But we who are on the earth
have, in our study of another planet, to regard it as having in a sense
two years. First, there is the time it takes, starting from a given
point in its orbit, to circle around the sun and return to that point.
This is known as its sidereal period, or year, and is so called from
_sidus_, meaning a star, because the only way to mark any point in
space is by a fixed star, and, as viewed from the sun, one revolution
of a planet would be from a given star back again to that star.
Then there is the time a planet takes, starting when it is in a
straight line with the earth and the sun in space, to return to the
place where the three bodies will be again in the same relative
position. This is known as its synodic period, or year. Synodic is from
our word synod, meaning a meeting or assembly, and the synodic year is
the time between two successive and similar meetings of these three
bodies. The sidereal year concerns the planet in its relation to the
sun; the synodic year, in its relation to the earth. The synodic year
is the only one that much concerns us while regarding the planets as
a part of the spectacle of the sky. It is the one that we know from
observation, while the sidereal year is mathematically computed.
The two periods, or years, are not of the same length, because the
sun with reference to the planet is always stationary, and the motion
resulting in the sidereal year is that of the planet only, while the
synodic year is the result of the movements of both the earth and the
planet, each, in its own orbit, being always in motion.
An inferior planet, situated as it is nearer to the sun than the earth
is, and so having a shorter orbit than the earth’s, will, when it
finishes its sidereal year and comes around to the point from which
it started, find the earth advanced from that position and will,
therefore, have to travel farther on in order to overtake it and come
into the same relative position from which they started, which makes
the time of its circuit with reference to the earth obviously longer
than with reference to the sun.
With the superior planets the case is just reversed. The earth is
the inside planet, or the one nearest the sun, and it must overtake
_them_. With one exception, they are all so far away from the sun and
move so slowly that it takes us but little more than one of our years
to overtake them and bring them into the same relative position with
us that they had when we started, while it requires many of our years
for any one of them to make a single circuit of the sun. Hence their
circuit with reference to the earth is shorter than with reference to
the sun.
Public-domain text, read in full here on John Shaqi.
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