Scientific American Supplement, No. 648, June 2, 1888.Various
Science
Scientific American Supplement, No. 648, June 2, 1888.
Various
Science -- Periodicals
Naturally we begin with the sun, and the oldest and most important problem
which the study of this body offers is the determination of its distance
from the earth in terrestrial units of measure. This distance is important
because the knowledge of all the phenomena of all the heavenly bodies,
except those of the moon, depend directly or indirectly on its value. The
problem of the sun's distance is difficult because the data given for
determining it are insufficient to enable the astronomer to apply the
principles of trigonometry directly to it. He is, therefore, compelled to
use indirect methods of solution, which, at best, give only approximations
to the true distance, arising chiefly from small errors in observation,
which, at the present time, seem unavoidable. A familiar illustration will
make our meaning clear. The knowledge we have of the sun's distance
depends on the accurate measurement of a small angle formed by drawing two
lines from a point at the sun to the extremities of the earth's radius.
That angle is called the sun's parallax. Ptolemy thought that this angle
was 3' of arc, but we now know that its value is very near 8.80" of arc,
and that the error of this amount from the true angle probably is not more
than 0.02". To measure this small angle has been the astronomer's great
trouble since the time of Aristarchus, and he does not yet know its value
accurately. His problem is like that of a surveyor attempting to measure a
ball, whose real diameter is one foot, at the distance of 4.4 miles
nearly; and unless he can determine the diameter of the ball so that he
shall not be uncertain in his measure to the amount of 0.03 of an inch,
his work will not add anything useful to present knowledge.
If we suppose the angle of parallax to be known, the computation of the
distance of a celestial body is easy. Multiply earth's radius by 206,265
(seconds of arc in the unit radius), and divide the product by the angle
of parallax in seconds of arc. The mean equatorial radius of the earth, as
given in Clark's Geodesy, is 3963.3 English miles. The sun's distance for
a parallax of 8.78" would be
206,265" × 3963.3
----------------- = 93,108,000 miles.
8.78"
For parallax of 8.80" = 92,897,000 miles.
For parallax of 8.82" = 92,686,000 miles.
The range of error in parallax, as here given, is 0.04", and the change of
the distance of the sun in allowing for this error is nearly half a
million of miles. If 8.80" be the assumed parallax, with ± 0.02" as
probable error, then the uncertainty of the sun's distance is still nearly
a quarter of a million of miles.
Public-domain text, read in full here on John Shaqi.
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