The sea west of Spitsbergen; the oceanographic observations of the Isachsen Spitsbergen Expedition in 1910 . e mentioned I. The temperature-curves of Figs. 5 and 6 (Sec-tions IV and VI) do not exhibit any such strikingirregularities in the intermediate strata (500 and600 metres) at the boundary between the observa-tions taken with the Nansen-thermometer and thosetaken with the reversing thermometer. The slightindications of a similar irregularity, which are notice-able, may be accounted for by the error of ° the Nansen-thermometer had later. Thereadings have naturally also to be co
The sea west of Spitsbergen; the oceanographic observations of the Isachsen Spitsbergen Expedition in 1910 . e mentioned I. The temperature-curves of Figs. 5 and 6 (Sec-tions IV and VI) do not exhibit any such strikingirregularities in the intermediate strata (500 and600 metres) at the boundary between the observa-tions taken with the Nansen-thermometer and thosetaken with the reversing thermometer. The slightindications of a similar irregularity, which are notice-able, may be accounted for by the error of ° the Nansen-thermometer had later. Thereadings have naturally also to be corrected for the error caused by theadiabatic cooling during the hauling up of the insulated water-bottle; but itdoes not amount to much in these observations, ° C. at most [ci~. V. , 1905, p. 16]. On the homeward voyage in September, Captain Isachsex had theobservations at some of the former stations repeated. Fig. 7 shows the igi2. No. 12. THE SEA WEST OF SPITSBERGEN. Fig. 6. Vertical Temperature-Curves of Sect. VI. Readings of Nansen-thermometer are not corrected. Om -1 100 \ 200 300 500.
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