Letters on Natural Magic; Addressed to Sir Walter Scott, Bart.Brewster, David
History
Letters on Natural Magic; Addressed to Sir Walter Scott, Bart.
Brewster, David
Scientific recreations
The reflected spectre of Dr. Buchan standing upon the cliff at
Brighton, arose from a cause to which we have not yet adverted. It was
obviously no shadow, for it is certain, from the locality, that the
rays of the sun fell upon the face of the cliff and upon his person at
an angle of about 73° from the perpendicular, so as to illuminate them
strongly. Now, there are two ways in which such an image may have been
reflected, namely, either from strata of air of variable density, or
from a vertical stratum of vapour, consisting of exceedingly minute
globules of water. Whenever light suffers refraction, either in passing
at once from one medium into another, or from one part of the same
medium into another of different density, a portion of it suffers
reflexion. If an object, therefore, were strongly illuminated, a
sufficiently distinct image, or rather shadow of it, might be seen by
reflexion from strata of air of different density. As the temperature
at which moisture is deposited in the atmosphere varies with the
density of the air, then at the same temperature moisture might be
depositing in a stratum of one density, while no deposition is taking
place in the adjacent stratum of a different density. Hence there would
exist, as it were in the air, a vertical wall or stratum of minute
globules of water, from the surface of which a sufficiently distinct
image of a highly illuminated object might be reflected. That this
is possible may be proved by breathing upon glass. If the particles
deposited upon the glass are large, then no distinct reflection will
take place; but if the particles be very small, we shall see a distinct
image formed by the surface of the aqueous film.
The phenomena of the Fata Morgana have been too imperfectly described
to enable us to offer a satisfactory explanation of them. The aërial
images are obviously those formed by unequal refraction. The pictures
seen on the sea may be either the aërial images reflected from its
surface, or from a stratum of dense vapour, or they may be the direct
reflexions from the objects themselves. The coloured images, as
described by Minasi, have never been seen in any analogous phenomena,
and require to be better described before they can be submitted to
scientific examination.
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