The sea west of Spitsbergen; the oceanographic observations of the Isachsen Spitsbergen Expedition in 1910 . Fig. 9. Vertical Temperature-Curves of July and September, 1910, for Stat. 29. -/• 0° r Z 3 +° 5 6 11 i 111) I Dm. 100 200 300 100 TJ-TT 3° *° Si F~7 -&- ;$ %SL. fOOO Figs. 11 -curves aredrawn for agreat manystations ofSections 1 toVI. All temperature-readings ofthe Nansen-thermometer hadbeen corrected by ?+- the densities were com-puted. The dots mark the den-sities in depths where thisthermometer was used, the cros-ses those of the reversing thermo-meter. There is a str
The sea west of Spitsbergen; the oceanographic observations of the Isachsen Spitsbergen Expedition in 1910 . Fig. 9. Vertical Temperature-Curves of July and September, 1910, for Stat. 29. -/• 0° r Z 3 +° 5 6 11 i 111) I Dm. 100 200 300 100 TJ-TT 3° *° Si F~7 -&- ;$ %SL. fOOO Figs. 11 -curves aredrawn for agreat manystations ofSections 1 toVI. All temperature-readings ofthe Nansen-thermometer hadbeen corrected by ?+- the densities were com-puted. The dots mark the den-sities in depths where thisthermometer was used, the cros-ses those of the reversing thermo-meter. There is a striking difference betweenthe curves of June, Stations 2—13 (Figs. 11 and12), and those of July, Stations 17—28 (Figs. 13—15). The latter curves continue their courseregularly downwards from the upper part, above500 metres, where the Nansen-thermometer wasused, to the lower part where the reversingthermometer was used. There are many smallirregularities in the curves which may chiefly be 1912. No. 12. THE SEA WEST OF SPITSBERGEN. Fig. 10. Temperature-Curves of July and September, due to inaccuracies of the salini1910, for Stat. 30. tjes; but not more in the mentio 2° y 4° 5° 6°Om c— €./i(.tgjo l^—
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