The Heavens Above: A Popular Handbook of AstronomyRolfe, W. J. (William James)
Science
The Heavens Above: A Popular Handbook of Astronomy
Rolfe, W. J. (William James)
Astronomy
232. _Brilliancy of Venus._--Next to the sun and moon, Venus is at times
the most brilliant object in the heavens, being bright enough to be seen
in daylight, and to cast a distinct shadow at night. Her brightness,
however, varies considerably, owing to her phases and to her varying
distance from the earth. She does not appear brightest when at full, for
she is then farthest from the earth, at superior conjunction; nor does
she appear brightest when nearest the earth, at inferior conjunction,
for her phase is then a thin crescent (see Fig. 258). She is most
conspicuous while passing from her greatest eastern elongation to her
greatest western elongation. After she has passed her eastern
elongation, she becomes brighter and brighter till she is within about
forty degrees of the sun. Her phase at this point in her orbit is shown
in Fig. 260. Her brilliancy then begins to wane, until she comes too
near the sun to be visible. When she re-appears on the west of the sun,
she again becomes more brilliant; and her brilliancy increases till she
is about forty degrees from the sun, when she is again at her brightest.
Venus passes from her greatest brilliancy as an evening star to her
greatest brilliancy as a morning star in about seventy-three days. She
has the same phase, and is at the same distance from the earth, in both
cases of maximum brilliancy. Of course, the brilliancy of Venus when at
the maximum varies somewhat from time to time, owing to the
eccentricities of the orbits of the earth and of Venus, which cause her
distance from the earth, at her phase of greatest brilliancy, to vary.
She is most brilliant when the phase of her greatest brilliancy occurs
when she is at her aphelion and the earth at its perihelion.
[Illustration: Fig. 260.]
233. _The Atmosphere and Surface of Venus._--Schröter believed that he
saw shadings and markings on Venus similar to those on Mercury,
indicating the presence of an atmosphere and of elevations on the
surface of the planet. Fig. 261 represents the surface of Venus as it
appeared to this astronomer. By watching certain markings on the disk of
Venus, Schröter came to the conclusion that Venus rotates on her axis in
about twenty-four hours.
[Illustration: Fig. 261.]
It is now generally conceded that Venus has a dense atmosphere; but
Schröter's observations of the spots on her disk have not been verified
by modern astronomers, and we really know nothing certainly of her
rotation.
234. _Transits of Venus._--When Venus happens to be near one of the
nodes of her orbit when she is in inferior conjunction, she makes a
transit across the sun's disk. These transits occur in pairs, separated
by an interval of over a hundred years. The two transits of each pair
are separated by an interval of eight years, the dates of the most
recent being 1874 and 1882. Venus, like Mercury, appears surrounded with
a border on passing across the sun's disk, as shown in Fig. 262.
[Illustration: Fig. 262.]
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