Is Mars habitable? A critical examination of Professor Percival Lowell's book "Mars and its canals," with an alternative explanationWallace, Alfred Russel
Science
Is Mars habitable? A critical examination of Professor Percival Lowell's book "Mars and its canals," with an alternative explanation
Wallace, Alfred Russel
Lowell, Percival, 1855-1916. Mars and its canals; Mars (Planet)
When we are presented with a complex problem depending on a great number
of imperfectly ascertained data, we may often check the results thus
obtained by the comparison of cases in which some of the more important
of these data are identical, while others are at a maximum or a minimum.
In the present case we can do this by a consideration of the Moon as
compared with the Earth and with Mars.
_Langley's Determination of the Moon's Temperature._
In the moon we see the conditions that prevail in Mars both exaggerated
and simplified. Mars has a very scanty atmosphere, the moon none at all,
or if there is one it is so excessively scanty that the most refined
observations have not detected it. All the complications arising from
the possible nature of the atmosphere, and its complex effects upon
reflection, absorption, and radiation are thus eliminated. The mean
distance of the moon from the sun being identical with that of the
earth, the total amount of heat intercepted must also be identical; only
in this case the whole of it reaches the surface instead of one-fourth
only, according to Mr. Lowell's estimate for the earth.
Now, by the most refined observations with his Bolometer, Mr. Langley
was able to determine the temperature of the moon's surface exposed to
undimmed sunshine for fourteen days together; and he found that, even in
that portion of it on which the sun was shining almost vertically, the
temperature rarely rose above the freezing point of water. However
extraordinary this result may seem, it is really a striking confirmation
of the accuracy of the general laws determining temperature which I have
endeavoured to explain in the preceding chapter. For the same surface
which has had fourteen days of sunshine has also had a preceding
fourteen days of darkness, during which the heat which it had
accumulated in its surface layers would have been lost by free radiation
into stellar space. It thus acquires during its day a maximum
temperature of only 491° F. absolute, while its minimum, after 14 days'
continuous radiation, must be very low, and is, with much reason,
supposed to approach the absolute zero.
_Rapid Loss of Heat by Radiation on the Earth._
Public-domain text, read in full here on John Shaqi.
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