The Trouvelot astronomical drawings manualTrouvelot, E. L. (Etienne Leopold)
Science
The Trouvelot astronomical drawings manual
Trouvelot, E. L. (Etienne Leopold)
Astronomy -- Pictorial works
From December 18th, 1877, when the Sun was about 41' above the plane of
the rings, to February 6th, 1878, the day of its passage through their
plane, the illuminated surface of this system gradually decreased in
breadth with the lowering of the Sun, until it was lost sight of,
February 5th, on the eve of the passage of the Sun through their plane.
The phenomenon in question consisted in the gradual invasion of their
illuminated surface by what appeared to be a black shadow, apparently
cast by the front part of the outer portion of the middle ring the
nearest to the Sun. On January 25th, when the elevation of the Sun above
the plane of the rings was reduced to 15', the shadow thus cast had
extended so far on their surface that it reached the shadow cast by the
globe on the opposite part of the ring in the east, and accordingly the
remaining portion of the illuminated surface of the eastern ansa then
appeared entirely disconnected from the ball, by a large dark gap,
corresponding in breadth to that of the globe's shadow on the rings. On
February 4th, when the Sun was only 5' above the plane of the rings,
their illuminated and only visible surface was reduced to a mere thread
of light, which on the 5th appeared broken into separate points. It is
evident that the phenomenon was not caused by the obliquity of the ring
as seen from our globe, since the elevation of the Earth above the plane
of the rings--which on December 18th was 3° 20'--was still 1° 20' on
the 4th of February. In ordinary circumstances, when the Sun is a little
more elevated, and the rings seen at this last angle, they appear quite
broad and conspicuous, and even the dark open space separating the dusky
ring from the planet is perfectly visible on the ansæ, where the
Earth's elevation above their plane is reduced to 40'. It is also
evident that the phenomenon was not to be attributed to the reduction of
the light which they received from the Sun, although the illumination in
February might be expected to be comparatively feeble, since the Sun
then shone upon the rings so obliquely; yet (on the supposition that
their surface is flat) they should have been illuminated throughout, and
if not very brightly, sufficiently so, at least, to make them visible
and as bright as was the narrow thread of light observed on the 4th of
February. The phenomenon actually observed may be explained most readily
by assuming, as other phenomena also indicate, that the surface of the
ring is not flat, but more elevated towards, or in the vicinity of its
outer border, from which place it slopes inwardly towards the planet. On
this assumption, it is evident that the elevated part of the ring the
nearest to the Sun would cast a shadow, which, with the increasing
obliquity of the Sun, would gradually cover the whole surface comprised
within the elevated part, and thus become invisible to us. Several
observations made by Bond and other observers undoubtedly show the same
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