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
“In so far as the _Tegetthoff_ with her hull and masts presented a
greater surface to the wind, the floe, on which it was imprisoned, would
necessarily receive an excess of movement in the direction of the wind.
If this excess formed an angle with the direction of the movement of the
ice, the ship’s floe would deviate to the side of the least resistance,
and drift according to the resultant between wind and resistance. Thus
it might be that the ship’s course deviated from the wind, even in a
direction opposed to it. But these anomalies certainly were not great,
and could not well be estimated, because the deviations which thus arose
depended on the direction of the wind, on the density and mass of the
ice, on causes, in fact, which could not be exhibited under numerical
relations.
“If we compare the statements, as given in the _Meteorological
Journal_,[21] concerning the ice-drift and ice-pressures, it is seen that
the maximum of both occurred in those parts of the sea in which the ship
was within the action of the ice coming from the Sea of Kara, and that
the greatest deviations in the ship’s course necessarily happened there.
“With respect to another abnormal deviation in the ship’s course, it
cannot be doubted that this depended on the vicinity of Franz-Josef Land,
towards which the masses of ice drifted under the action of continuous
south-west winds; and were again driven back, thus forming a circle
in their movement. It would seem natural to assume the existence of a
sea-current in order to explain this peculiarity; but the configuration
of that land and its coasts, or the greater or lesser amount of
immovable ice, or, lastly, the prevailing winds in those regions,
may have influenced the direction of the movement of the ice, and
consequently of the ship’s course.
“If we consider the prevalence of winds, as furnished by Weyprecht’s
observations for more than two years, we find south-west winds prevailing
in the southern part of the seas that were navigated, and north-east
winds in the northern part of those seas.
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