The sea west of Spitsbergen; the oceanographic observations of the Isachsen Spitsbergen Expedition in 1910 . 800. BJORN HELLAND-HANSEN AND NANSEN. Fig. 13. Curves of Density (at) for Stats. 25 — 28 (Sect. IV). the densities of the up- 2B0U 17-90 27-80 27-70 2760 2750 z7,o per parts of the curves of June have to be re-duced in order to givethe curves probableshapes. Taking the sa-linities to be fairly correct, it is then possibleto determine how much the temperature-read-ings of the Nansen-thermometer have to beraised in order to give the probable densi-ties thus found. The ob
The sea west of Spitsbergen; the oceanographic observations of the Isachsen Spitsbergen Expedition in 1910 . 800. BJORN HELLAND-HANSEN AND NANSEN. Fig. 13. Curves of Density (at) for Stats. 25 — 28 (Sect. IV). the densities of the up- 2B0U 17-90 27-80 27-70 2760 2750 z7,o per parts of the curves of June have to be re-duced in order to givethe curves probableshapes. Taking the sa-linities to be fairly correct, it is then possibleto determine how much the temperature-read-ings of the Nansen-thermometer have to beraised in order to give the probable densi-ties thus found. The observations of the temperatures ofthe sea-surface were made with a specialthermometer which was immersed in the watertaken from the sea-surface with an ordinarybucket. Provided that these observations havebeen fairly correct and that the salinities found aretrustworthy, the densities of the surface-water give alimit below which the densities of the underlyingstrata may not be reduced by the raising of the tem-peratures taken with the Nansen-thermometer, notconsidering small irregularities that may arise fro
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Keywords: ., bookauthornansenfr, bookcentury1900, bookdecade1910, bookyear1912
