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
In the case of the sun the distance concerned is so great (about 400
times that of the moon) that the parallax produced by viewing it from
different points on the earth is too small to be certainly measured, and
a modification of the method has to be employed. One such modification,
which has been much used, depends upon the fact that the planet Venus,
being nearer the sun than the earth is, appears, at certain times,
passing directly over the face of the sun. This is called a transit of
Venus. During a transit, Venus is between three and four times nearer
the earth than the sun is, and consequently its parallactic
displacement, when viewed from widely separated points on the earth, is
much greater than that of the sun. One of the ways in which the
astronomer takes advantage of this fact is shown in Fig. 13. Let A and B
be two points on opposite sides of the earth, but both somewhere near
the equator. As Venus swings along in its orbit to pass between the
earth and the sun, it will manifestly be seen just touching the sun's
edge sooner from A than from B. The observer at A notes with extreme
accuracy the exact moment when he sees Venus apparently touch the sun.
Several minutes later, the observer at B will see the same phenomenon,
and he also notes accurately the time of the apparent contact. Now,
since we know from ordinary observation the time that Venus requires to
make one complete circuit of its orbit, we can, by simple proportion,
calculate, from the time that it takes to pass from v to v^1, the
angular distance between the lines A S and B S, or in other words the
size of the angle at S, which is equal to the parallactic displacement
of the sun, as seen from opposite ends of the earth's diameter. Knowing,
to begin with, the distance between A and B, we have the means of
determining the length of all the other lines in the triangle, and hence
the distance of the sun. This process is known as Delisle's method.
There is another method, called Halley's, but in a brief treatise of
this kind we cannot enter into a description of it. It suffices to say
that both depend upon the same fundamental principles.
[Illustration:
_Fig. 13. Parallax of the Sun from Transit of Venus_.
(For description see text.)
]
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