The sea west of Spitsbergen; the oceanographic observations of the Isachsen Spitsbergen Expedition in 1910 . Fig. 20. Curves of Density (/() for Stat. 27-80 27-70 27-60 27-50 WD: ZOO. tember 5th and 6th, 1900) and of Isachsens Stats. 3 and 4 of Sep-tember 7th, 1910. All these curves have a striking resemblance to eachother in shape, and also to the corrected curves of June 25th, 1910 (seeFig. 25), while the curves based upon the unaltered temperature-readingsof the Nansen-thermometer of June 25th, 1910, differ strikingly in theirshapes (see Figs. 7 and 8) from all other curves. 1912. N
The sea west of Spitsbergen; the oceanographic observations of the Isachsen Spitsbergen Expedition in 1910 . Fig. 20. Curves of Density (/() for Stat. 27-80 27-70 27-60 27-50 WD: ZOO. tember 5th and 6th, 1900) and of Isachsens Stats. 3 and 4 of Sep-tember 7th, 1910. All these curves have a striking resemblance to eachother in shape, and also to the corrected curves of June 25th, 1910 (seeFig. 25), while the curves based upon the unaltered temperature-readingsof the Nansen-thermometer of June 25th, 1910, differ strikingly in theirshapes (see Figs. 7 and 8) from all other curves. 1912. No. 12. THE SEA WEST OF SPITSBERGEN. 13 The Spitsbergen Atlantic Current. The oceanographic observations made during the cruise of the Farmin the summer of 1910 are especially valuable for the stud) of the Spits-bergen Atlantic Current. It was chiefly with this aim in view that theplan of the oceanographic work of the Farm was laid, when Capt. Isachsendiscussed it with the writers beforehand. It was thought to be of muchinterest to have this but little known continuation of the Norwegian At-lantic Current thoroughly investigated. Our knowledge of the Spitsbergen Atlantic Current had hi
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Keywords: ., bookauthornansenfr, bookcentury1900, bookdecade1910, bookyear1912
