Scientific American Supplement, No. 443, June 28, 1884Various
Science
Scientific American Supplement, No. 443, June 28, 1884
Various
Science -- Periodicals
Lord Rosse's later observations modified his conclusions, to some
extent, showing that he had at first underestimated the percentage of
simple reflected heat, but without causing him to make any radical
change in his ideas as to the maximum heat of the moon's surface.
For some time, however, there has been a growing skepticism among
astronomers, relating not so much to the correctness of his measures
as to the computations by which he inferred the high percentage of
obscure radiated beat compared with the reflected heat, and so deduced
the high temperature of lunar noon.
Professor Langley, who is now engaged in investigating the subject,
finds himself compelled to believe that the lunar surface never gets
even comfortably warm--because it has no blanket. It receives heat, it
is true, from the sun, and probably some twenty-five or thirty per
cent. more than the earth, since there are no clouds and no air to
absorb a large proportion of the incident rays; but, at the same time,
there is nothing to retain the heat, and prevent the radiation into
space as soon as the surface begins to warm. We have not yet the data
to determine exactly how much the temperature of the lunar rocks would
have to be raised above the absolute zero (-273 deg. C. or -459 deg. F.) in
order that they might throw off into space as much heat in a second as
they would get from the sun in a second. But Professor Langley's
observations, made on Mount Whitney at an elevation of fifteen
thousand feet, when the barometer stood at seventeen inches
(indicating that about fifty-seven per cent. of the air was still
above him), showed that rocks exposed to the perpendicular rays of the
sun were not heated to any such extent as those at the base of the
mountain similarly exposed; and the difference was so great as to make
it almost certain that a mass of rock not covered by a reasonably
dense atmosphere could never attain a temperature of even 200 deg. or 300 deg.
F. under solar radiation, however long continued.
It must, in fact, be considered at present extremely doubtful whether
any portion of the moon's surface ever reaches a temperature as high
as -100 deg..
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account