A Popular History of Astronomy During the Nineteenth Century: Fourth EditionClerke, Agnes M. (Agnes Mary)
History
A Popular History of Astronomy During the Nineteenth Century: Fourth Edition
Clerke, Agnes M. (Agnes Mary)
Astronomy -- History -- 19th century
Using an ingenious apparatus for viewing simultaneously the spectrum
from both sides of the sun, Professor Hastings noticed at Caroline
Island alternations, with the advance of the moon, in the respective
heights above the right and left solar limbs of the coronal green line,
which were thought to imply that the corona, with its rifts and sheaves
and "tangled hanks" of rays, is, after all, merely an illusive
appearance produced by the diffraction of sunlight at the moon's
edge.[552] But the observation was assuredly misleading or
misinterpreted. Atmospheric _diffusion_ may indeed, under favouring
circumstances, be effective in deceptively enlarging solar appendages;
but always to a very limited extent.
The controversy is an old one as to the part played by our air in
producing the radiance visible round the eclipsed sun. In its original
form, it is true, it came to an end when Professor Harkness, in
1869,[553] pointed out that the shadow of the moon falls equally over
the air and on the earth, and that if the sun had no luminous
appendages, a circular space of almost absolute darkness would
consequently surround the apparent places of the superposed sun and
moon. Mr. Proctor,[554] with his usual ability, impressed this
mathematically certain truth upon public attention; and Sir John
Herschel calculated that the diameter of the "negative halo" thus
produced would be, in general, no less than 23°.
But about the same time a noteworthy circumstance relating to the state
of things in the solar vicinity was brought into view. On February 11,
1869, Messrs. Frankland and Lockyer communicated to the Royal Society a
series of experiments on gaseous spectra under varying conditions of
heat and density, leading them to the conclusion that the higher solar
prominences exist in a medium of excessive tenuity, and that even at the
base of the chromosphere the pressure is far below that at the earth's
surface.[555] This inference was fully borne out by the researches of
Wüllner; and Janssen expressed the opinion that the chromospheric gases
are rarefied almost to the degree of an air-pump vacuum.[556] Hence was
derived a general and fully justified conviction that there could be
outside, and incumbent upon the chromosphere, no such vast atmosphere as
the corona appeared to represent. Upon the strength of which conviction
the "glare" theory entered, chiefly under the auspices of Sir Norman
Lockyer, upon the second stage of its existence.
Public-domain text, read in full here on John Shaqi.
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