A voyage to Spitzbergen: containing an account of that country, of the zoology of the North; of the Shetland Islands; and of the whale fisheryLaing, John (Surgeon)
History
A voyage to Spitzbergen: containing an account of that country, of the zoology of the North; of the Shetland Islands; and of the whale fishery
Laing, John (Surgeon)
Animals -- Arctic regions; Shetland (Scotland) -- Description and travel; Svalbard (Norway) -- Description and travel; Whaling
Mr. Marten has affirmed, that the sun here, at midnight, appears
with all the faintness of the moon; but his assertion has not been
corroborated by the experience of subsequent voyagers. During my
stay in this country, in 1806 and 1807, distinction between day and
night was almost completely lost. Any perceptible difference between
the splendour and radiance of the mid-day and mid-night sun, in
clear weather, (if these expressions may be used,) arose only from a
different degree of altitude. Some of our most experienced Greenland
sailors, when called upon deck, have frequently asked me whether it
was day or night; and I have often seen them obliged, even in clear
sun-shine, to consult the quadrant on this head. I may add, that
Captain Phipps has also contradicted Mr. Marten in the most positive
manner.
The temperature here is extremely fluctuating. Sometimes the heat is so
great as to melt the pitch on the decks and cordage of the vessels, and
in a few minutes after, succeed high winds, snow, and frost. The sky,
even in calm and serene weather, is covered with dense white clouds,
the repositories of the snow so often falling.
The degree of heat experienced in these northern latitudes being
so much greater than is experienced in the same latitudes in the
southern hemisphere, is supposed to proceed from the greater quantity
of land in the north reflecting the rays of the sun, which in the
south are absorbed by the ocean. Whatever hypothesis may be adduced
to account for the greater temperature of the north, the fact itself
is indisputable. Terra del Fuego, situated only in fifty-five degrees
south latitude, is extremely cold; and Captain Cook could not penetrate
farther than the seventy-first degree of latitude, a distance far short
of what the Greenland ships are every year in the habit of sailing
towards the other Pole.
Thunder and lightning are unknown at Spitzbergen, or at least are
extremely rare. Forster supposes that the electric exhalations in a
country so much covered with snow must be very few, and these so much
consumed by the frequency of the _Aurora Borealis_, that there is
never collected at one time a quantity of fluid sufficient to produce
thunder and lightning. That luminous appearance, so often observed
during a storm in this country, he alleges to be the effect of volcanic
eruptions; though this, I confess, seems to me extremely problematical.
Vid. Forster’s _Hist. Voyages_, p. 486.
There is a great diversity among the accounts given by different
travellers, of the forms assumed by the new fallen snow in this
country. During hard frost, I always observed that the flakes closely
resembled an asterisk with six points. As the temperature varied,
their appearance was changed, which may, perhaps, serve to explain the
differences alluded to.
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