30 



BJØRN HELLAND-HAXSEN AND FRIDTJOF NANSEN. 



M.-N. Kl. 



M -/' 



position than Stat. 3, 

 while Stat. 64 had a 

 / more westerly posi- 

 tion than Stat. 4. 



The curves of 

 both Hjort's stations 

 indicate in all depths 

 much lower temperatures 

 than the curves of Stats. 3 

 and 4 of September 7th, 

 1910. Fig. 23 shows a simi- 

 lar difference between the 

 curves of Hjort's Stats. 62 

 and 63 of September 5th, 1900, and the 

 curves of Isachsen's Stats, i and 2 of lune 



iOOOi^ 



that Hjort's temperatu- 

 res are higher, and 

 this is naturally due to 

 the heating of the sur- 

 face during the summer. 

 In Fig. 22 the verti- 

 cal temperature-curves of Makaroft's 

 Stats. 33 and 34 (Ma 33 and Ma 34) 

 of September 4th, 1899, are repre- 

 sented. The latitude of Isachsen's 



