that we can explain them on
the same general principles that we have applied to terrestrial
phenomena. There can be but little doubt about the existence of a solar
atmosphere, and, reasoning from analogy, the constituent elements of the
sun must partake of the nature of other planetary matter. That there are
bodies in our system possessing the same elements as our earth, is
proved by the composition of meteoric masses, which, whether they are
independent bodies of the system, or fragments of an exploded planet, or
projected from lunar volcanoes, is of little consequence; they show that
the same elements are distributed to other bodies of the system,
although not necessarily in the same proportions. The gaseous matter of
the sun's atmosphere may, therefore, be safely considered as vapors
condensable by cold, and the formation of vortices over the surface of
this atmosphere, brings down the ether, and causes it to intermingle
with this atmosphere. But, from the immensely rapid motion of the polar
current of the solar vortex, this ether may be considered to enter the
atmosphere of the sun with the temperature of space.
Sir John Herschel, in commenting on the theory of Mr. Redfield before
the British Association, convened at Newcastle in 1838,[35] suggested an
analogy to terrestrial hurricanes, from a suspected rotation and
progressive motion in these spots. From their rapid formation, change of
shape, and diameter, this view is allowable, and, taken in conjunction
with the action of the ethereal currents, will account for all the
phenomena. The nucleus of the spot is dense, like the nucleus of a storm
on the earth, and surrounded by a penumbon precisely as our storms are
fringed with lighter clouds, permitting the light of the sun to
penetrate. And, it has been observed, that these spots seem to follow
one another in lines on the same parallel of solar latitude (or nearly
the same), exactly as we have determined the action of the vortices on
the surface of the earth from observation. These spots are never found
in very high latitudes--not much above 30d from the solar equator. If we
consider this equator to be but slightly inclined to the plane of the
vortex, this latitude would be the general position of the lateral solar
vortices, and, in fact, be confined principally to a belt on each side
of the equator, between 15d and 30d of solar latitude, rather than at
the equator itself. This, it is needless to say, is actually
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