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
It is possible that the title and contents of this volume may allure
to its perusal some who look forward to exposure to dangers such
as those which are here described. They surely will not deem it
intrusive to be reminded that the most important preparation for
such undertakings, as well as for the whole of life, is to surrender
the heart to that Saviour who has died to redeem his servants from
guilt and ruin. The pardon and peace which he freely confers on all
who come to him, are the only safe comforts of a departing soul. It
is his blood only that cleanses from all sin; it is his Spirit that
renews and sanctifies the mind; and whatever pain or accident may
befal the body, there can be “no condemnation” in time or in eternity
“to them which are in Christ Jesus.” The message of God to man is the
offer of a free salvation, through the death of his glorious Son.
This offer must determine the eternal condition of all to whom it is
in God’s mercy revealed. “God so loved the world, that he gave his
only begotten Son, that whosoever believeth in him should not perish,
but have everlasting life!” Reader, do you understand, and have you
accepted, this gracious message?
FOOTNOTES:
[1] Now sir John Ross and sir Edward Parry.
CHAPTER IV.
OBSERVATIONS ON THE ATMOSPHEROLOGY OF THE ARCTIC REGIONS,
PARTICULARLY RELATING TO SPITZBERGEN AND THE ADJACENT GREENLAND SEA.
In treating of the subject of this chapter, our remarks shall, in
the first instance, relate to the _climate of the Arctic Regions
and the general effects of cold_. In the autumn and spring seasons,
the climate of Spitzbergen and its adjacent sea is variable and
tempestuous. The temperature passes through its extreme range, which,
probably, exceeds fifty degrees in the same season, or even in the
same month, with a rapidity unknown in countries situate within the
temperate zones. North, west, and east winds bring with them the
extreme cold of the icy regions immediately surrounding the Pole,
whilst a shift of wind to the south-west, south, or south-east,
elevates the temperature towards that of the neighbouring seas.
An arctic winter consists of the accumulation of almost everything
among atmospheric phenomena that is disagreeable to the feelings,
together with the privation of those bounties of Heaven with which
other parts of the earth, in happier climates, are so plentifully
supplied. During the whole of the winter months, the cheering rays of
the sun are neither seen nor felt, and there are occasional storms of
wind and snow.
The most severe cold, says Crantz, that occurs in Greenland, sets in,
as in temperate climates, “after the new year; and is so piercing
in February and March, that the stones split in twain, and the sea
reeks like an oven.” On the return of the sun, the months of May,
June, and August, are even occasionally pleasant; but with July, and
partially with June and August, the densest fogs prevail, which are
more depressing to the spirits than even intense cold.
Public-domain text, read in full here on John Shaqi.
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