On the Connexion of the Physical SciencesSomerville, Mary
Science
On the Connexion of the Physical Sciences
Somerville, Mary
Physical sciences; Science
Some very singular appearances occur from the accidental expansion or
condensation of the strata of the atmosphere contiguous to the surface
of the earth, by which distant objects, instead of being elevated, are
depressed. Sometimes, being at once both elevated and depressed, they
appear double, one of the images being direct, and the other inverted.
In consequence of the upper edges of the sun and moon being less
refracted than the lower, they often appear to be oval when near the
horizon. The looming also or elevation of coasts, mountains, and ships,
when viewed across the sea, arises from unusual refraction. A friend of
the author’s, while standing on the plains of Hindostan, saw the whole
upper chain of the Himalaya Mountains start into view, from a sudden
change in the density of the air, occasioned by a heavy shower after a
very long course of dry and hot weather. Single and double images of
objects at sea, arising from sudden changes of temperature which are not
so soon communicated to the water on account of its density as to the
air, occur more rarely and are of shorter duration than similar
appearances on land. In 1818 Captain Scoresby, whose observations on the
phenomena of the polar seas are so valuable, recognised his father’s
ship by its inverted image in the air, although the vessel itself was
below the horizon. He afterwards found that she was seventeen miles
beyond the horizon, and thirty miles distant. Two images are sometimes
seen suspended in the air over a ship, one direct and the other
inverted, with their topmasts or their hulls meeting, according as the
inverted image is above or below the direct image (N. 193). Dr.
Wollaston has proved that these appearances are owing to the refraction
of the rays through media of different densities, by the very simple
experiment of looking along a red-hot poker at a distant object. Two
images are seen, one direct and another inverted, in consequence of the
change induced by the heat in the density of the adjacent air. He
produced the same effect by a saline or saccharine solution with water
and spirit of wine floating upon it (N. 194).
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