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Thus the constitution of the water in the deeper strata
and at the bottom was found to be almost unchanged in 1875,
76 & 78, and yet we know that, from a nautic point of view,
the condition of the Kara Sea was very different in 1876 from
in 1875 or 1878.
I next wish to call attention to the important fact, that
the same constitution of the deeper vvater-strata with regard
to saltness and temperature also prevails in that part of the
Barentz Sea west of the Waigatch and Novaya Zemlya, as may
be seen from the following observations by the Swedish
expedition, 1875, and the Holland, 1881.
Western entrance to the Matochkin strait; 13th July 1875.
Depth Temperature. Saltness [anal, by Ekman]
0 m. + 6J.i C 3.03 p. c.
23 m. + 4q.2 C
35 m. (bottom) 3.38 p. c.
Ibid. Lat. 73°5’; Long. 52° 14’; 6th August 1881.
Depth. Temperature.
0 m. + 3°.o C [Holland expedition]
64 m. (bottom) —0’.4 C * »
Barentz Sea, west of Besimannaya Bay, Lat, 72° 43’; Long.
52°; 30th June 1875.
Depth. Temperature. Saltness [anal, by Ekman].
0 in. + 0°.e C 3.27 p. c.
17.8 111. ––- 1°.4 C ––-
35.6 m. — 1°.9 C ––-
53.4 m. —1°. 7 C ––-
89 m. (bottom)–––––––- 3.4.2 p. c.
Barentz Sea, Lat. 70°49’; Long. 50°47’; 26th July 1881.
Depth Temperature.
0 m. — 03.8 C [Holland expedition]
120 ni. (bottom) —1°.4 C » »
Some miles farther to the south-west a very different
result was obtained
Barentz Sea, Lat, 70°30’; Long. 49°41’; 29th 1881.
Depth. Temperature.
0 m. + 5°.7 C [Holland expedition]
96 m. (bottom) + 3°.8 C » »
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