Meteorology; or, Weather ExplainedM'Pherson, J. G. (John Gordon)
Science
Meteorology; or, Weather Explained
M'Pherson, J. G. (John Gordon)
Meteorology
One of the most interesting experiments, without apparatus, which you can
make is in connection with the formation of hoar-frost, when there is no
snow on the ground, in very cold weather. If it has been a bright, clear,
sunny day in January, the effect can be better observed. Look over the
garden, grass, and walks on the morning after the intense cold of the
night; big plane-tree leaves may be found scattered over the place. You
see little or no hoar-frost on the _upper_ surface of the leaves. But turn
up the surface next the earth, or the road, or the grass, and what do you
see? You have only to handle the leaf in this way to be brightly
astonished. A thick white coating of hoar-frost, as thick as a layer of
snow, is on the _under_ surface. If a number of leaves have been
overlapping each other, there will be no coating of hoar-frost under the
top leaves; but when you reach the lowest layer, next the bare ground, you
will find the hoar-frost on the under surface of the leaves. Now that is
positive proof that the hoar-frost has not fallen from the air, but has
risen from the earth.
The sun's heat on the previous day warmed the earth. This heat the earth
retained till evening. As the air chilled, the water-vapour from the
warmer earth rose from its surface, and was arrested by the cold surface
of the leaves. So cold was that surface that it froze the water-vapour
when rising from the earth, and formed hoar-frost in very large
quantities. When this happens later on in the season, one may be almost
sure of having rain in the forenoon.
Public-domain text, read in full here on John Shaqi.
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