The sea west of Spitsbergen; the oceanographic observations of the Isachsen Spitsbergen Expedition in 1910 . position than Stat. 3,while Stat. 64 had amore westerly posi-tion than Stat. 4. The curves ofboth Hjorts stationsindicate in all depthsmuch lower temperaturesthan the curves of Stats. 3and 4 of September 7th,1910. Fig. 23 shows a simi-lar difference between thecurves of Hjorts Stats. 62and 63 of September 5th, 1900, and thecurves of Isachsens Stats. 1 and 2 of June25th, 1910, although the latter observa-tions were taken 72 days earlier in theseason. It is only in the upper 50 metres Fig

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The sea west of Spitsbergen; the oceanographic observations of the Isachsen Spitsbergen Expedition in 1910 . position than Stat. 3,while Stat. 64 had amore westerly posi-tion than Stat. 4. The curves ofboth Hjorts stationsindicate in all depthsmuch lower temperaturesthan the curves of Stats. 3and 4 of September 7th,1910. Fig. 23 shows a simi-lar difference between thecurves of Hjorts Stats. 62and 63 of September 5th, 1900, and thecurves of Isachsens Stats. 1 and 2 of June25th, 1910, although the latter observa-tions were taken 72 days earlier in theseason. It is only in the upper 50 metres Fig. 23. f J w. tOOOi- that Hjorts temperatu-res are higher, andthis is naturally due tothe heating of the sur-face during the Fig. 22 the verti-cal temperature-curves of MakarofPsStats. 33 and 34 (Ma 33 and Ma 34)of September 4th, 1899, are repre-sented. The latitude of Isachsens 1912. No. 12. THE SEA WEST OF SPITSBERGEN. 31 too-

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