New lands within the Arctic circle: Narrative of the discoveries of the Austrian ship "Tegetthoff" in the years 1872-1874Payer, Julius
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New lands within the Arctic circle: Narrative of the discoveries of the Austrian ship "Tegetthoff" in the years 1872-1874
Payer, Julius
Admiral Tegetthoff (Ship); Arctic regions; Franz Josef Land (Russia) -- Discovery and exploration
3. The season of the year for sledging must depend on the climate of
particular Arctic localities, and the capacity of the men to endure low
temperatures during the night-camping, and driving snow during the march.
It is advisable, when more than one year is to be spent in the ice, to
begin the more extended sledge-journeys in the first year, because the
capacities of Europeans to endure cold rather decrease than increase.
Sir John Ross, for example, says that his people at the beginning of a
third winter were incapable of bearing hardships, especially those of
travelling on the ice. The best season for sledging must always be that
time of the year when snow-storms are infrequent, for even a healthy and
seasoned party will more easily confront a very low temperature than
driving snow-storms. As a rule, these conditions are found most perfectly
in autumn; and I do not understand the objection which Hayes makes to
this season as being the most damp; whereas as a matter of fact it is the
least so. Autumn journeys are preferable to those in spring, both with
respect to climate and the state of the road; only they must be commenced
early, on account of the rapidly decreasing length of the days.[27] The
darkness of winter puts an end to all sledging, and the excessive cold of
spring renders it difficult. Summer makes it impossible by breaking up
the land-ice, or impedes it by transforming the snow into thaw-water and
sludge. Next to autumn, therefore, the latter part of March, all April,
and a part of May, are most adapted for this purpose. It must at the same
time be remarked, that Captain Lyon (1822) and Dr. Kane regarded March as
peculiarly dangerous on account of the prevalence of storms.
4. Next to the season, the state of the snow road, depending on the
hardening action of wind and cold, has to be considered. The cold
should not vary more than from -2° to -24° F., because greater frost
transforms the smooth evaporating surface of snow into a rough plain,
bestrewed with sharp pointed crystals, so that the sledge instead of
gliding along encounters the friction, as if of a sandstone surface,
and stops at the least obstacle. Snow of an ivory-like smoothness rarely
occurs; on the contrary, we find the snow in deep layers as fine as
powder, into which we sink knee-deep, or among barriers of hummocks,
miles in extent, which impose enormous détours in the transport of the
baggage. During the journey from 2° to 13° below zero F. constitutes
the pleasantest temperature, and even the nights, under this condition,
are passed without inconvenience by a party inured to exposure.
Snow-storms, however, in their mildest form—snow-drifting—are, at this
moderate temperature, distressing and dangerous. In fact, among all the
contingencies which may occur during a Polar expedition, there is no
severer test of enduring perseverance than dragging a sledge in the face
of drifting snow at a temperature from 13° to 35° below zero F.
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