The sea west of Spitsbergen; the oceanographic observations of the Isachsen Spitsbergen Expedition in 1910 . 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-. Stats. 3 and 4 was re- Fig- 24. spectivelv only about27 and 14 minutesmore southerly thanMakarofFs Stat. 33,while they were about ?00:-i° 33 and i° 46 morenortherl
The sea west of Spitsbergen; the oceanographic observations of the Isachsen Spitsbergen Expedition in 1910 . 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-. Stats. 3 and 4 was re- Fig- 24. spectivelv only about27 and 14 minutesmore southerly thanMakarofFs Stat. 33,while they were about ?00:-i° 33 and i° 46 morenortherly than Maka- o^roffs Stat. 34. Themeridian of Makaroffs ^.0Gstation 33 was be-tween those of Stats. 3 and 4, and that of his Stat. 34 one degree morewesterly than Stat. 4 (see Fig. 211 The observations at all four stationswere taken in the first week of September of 1899 and 1910. Both Maka-roffs curves show much lower temperatures than those of Stats. 3 and 4,especially in depths of less than 400 metres. The mean temperature of the water between 50 and 450 metres atMakaroffs two stations was C. while the corresponding mean tempera-ture for Stats. 3 and 4 was ° C. If these temperatures were compar-able, the Atlantic water should thus have been about C. colder in 1899 than in 1910. The vertical tempera-ture-curves of MakaroffsStats. 5, 6, and 7 (Fig. 21,Ma 5, Ma 6, and Ma 7) ofJune 30th and July ist,1899, sh
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