The Arctic regions and the northern whale-fisheryScoresby, William
History
The Arctic regions and the northern whale-fishery
Scoresby, William
Arctic regions; Whaling -- Arctic regions
This remarkable force of the sun’s rays is accompanied with a
corresponding intensity of light. A person placed in the centre of
a field or other compact body of ice, under a cloudless atmosphere
and elevated sun, experiences such an extraordinary intensity of
light, that if it be encountered for any length of time, is not only
productive of a most painful sensation in the eyes, but sometimes
of temporary, or even, as I have heard, of permanent blindness.
Under such circumstances, the use of green glasses affords a most
agreeable relief. Some of the Indians of North America defend their
eyes by the use of a kind of wooden spectacles, having, instead of
glasses, a narrow perpendicular slit opposite to each eye. This
simple contrivance, which intercepts, perhaps, nine-tenths of the
light that would reach a naked eye, prevents any painful consequences
in the most intense reflection of light that ever occurs.
The constant light of the sun during the summer prevents the stars
from being seen; and this, together with the frequency of cloudy
or foggy weather, rarely admits a sight of the moon. Hence, the
longitude, which is of such essential importance in navigation, can
seldom be determined by lunar observations. Chronometers, therefore,
though but little used by the whale-fishers, become of enhanced
value; and even a good watch, well regulated, will, where the degrees
of longitude are so very contracted, point out the meridianal
situation of the ship for short intervals, with a very tolerable
degree of accuracy.
Though the air in the arctic seas is generally in a state of
dampness, approaching to complete saturation, yet the absolute
quantity of moisture cannot, when the cold is very excessive, be
considerable. It is remarked, that vessels are less apt to rust here
than in any other climate; and this observation, if we consider the
relative humidity of the atmosphere as indicated by the hygrometer,
is certainly correct; but though the air in the Polar regions is
generally damp, yet it is probable there is no habitable situation in
the known world in which such a degree of actual dryness prevails, as
in a house or in the cabin of a ship, well heated, when the external
air is intensely cold. The wainscoting of the cabin of a ship in cold
weather sometimes shrinks, in consequence of the uncommon dryness, as
much as half an inch in a panel of about fifteen inches broad, being
equal to one-thirtieth of the breadth; but, on returning to Britain,
the same panel expands again to almost its original dimensions.
Public-domain text, read in full here on John Shaqi.
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