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
When a body is in the zenith, since a ray of light from it enters the
atmosphere at right angles to the refracting medium, it suffers no
refraction. Consequently, the position of the heavenly bodies, when in
the zenith, is not changed by refraction, while, near the horizon, where
a ray of light strikes the medium very obliquely, and traverses the
atmosphere through its densest part, the refraction is greatest. The
whole amount of refraction, when a body is in the horizon, is
thirty-four minutes; while, at only an elevation of one degree, the
refraction is but twenty-four minutes; and at forty-five degrees, it is
scarcely a single minute. Hence it is always important to make our
observations on the heavenly bodies when they are at as great an
elevation as possible above the horizon, being then less affected by
refraction than at lower altitudes.
Since the whole amount of refraction near the horizon exceeds
thirty-three minutes, and the diameters of the sun and moon are
severally less than this, these luminaries are in view both before they
have actually risen and after they have set.
The rapid increase of refraction near the horizon is strikingly evinced
by the _oval_ figure which the sun assumes when near the horizon, and
which is seen to the greatest advantage when light clouds enable us to
view the solar disk. Were all parts of the sun equally raised by
refraction, there would be no change of figure; but, since the lower
side is more refracted than the upper, the effect is to shorten the
vertical diameter, and thus to give the disk an oval form. This effect
is particularly remarkable when the sun, at his rising or setting, is
observed from the top of a mountain, or at an elevation near the
seashore; for in such situations, the rays of light make a greater angle
than ordinary with a perpendicular to the refracting medium, and the
amount of refraction is proportionally greater. In some cases of this
kind, the shortening of the vertical diameter of the sun has been
observed to amount to six minutes, or about one fifth of the whole.
Public-domain text, read in full here on John Shaqi.
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