Hydrographical Observations from the Danmark Expedition. 



361 



This agrees with the observations already mentioned, that the 

 water most cooled is found in the western part of the true Polar Cur- 



DeJlsity 14.00 25 50 75 ZSOO 25 SO 7S 26,00 25 50 75 27.00 25 50 75 28 00 



Salinity /OO 29-00 25 50 75 50w 25 SO 75 3100 25 SO 75 32 00 25 SO 75 35oO 2S SO 7S I4a0 25 SO 75 35oO 



TempejatuT ^-2' » Ç 3.„i ij' ' i t г 2 ч б ь +1 ' г t § s +Z'_ 



Station LXXV. 



PeHSity 2*00 25 50 75 2S00 25 50 7S 26oO 25 



Saiinity %0 29-00 25 50 75 ÎO-00 25 So 75 31-00 25 50 75 3200 25 



Temi 



75 27,00 25 50 75 28-00 



75 3300 25 50 75 ЪЧОО 25 



Г 2 » С « +2 



50 



ч> '300 



3500 



Station LX XVI. 



Density ZÎ.00 2s 

 Salmity %o 29 oo 2s 



2*00 25 

 bO-OO 25 



re 25 00 25 

 7S SIOO 26 



-r 



75 26.00 25 

 7S 32-00 25 



o 



27.00 25 



50 



75 



28 00 





55-00 ;s 



50 



75 



5too 



25 



8 *V 



2 



Ч 



6 



8 



*Z' 



75 Î5-0O 



100 







*■- - 





■~"*" 



"^"1 



T 



fe== 



--— 



----- 



,-,!--' 







.-_,. 



^-v 



--0-- 



--,, 









































/ 

























*., 



'- 



'^^ 

























s 



























'^. 





"" 



-Ч, 











§200 











v^ 



--^ 



























\_ 







V, 



























■ — 



-* 





__ 

















s. 





^ 



>,_ 





500 































-^ 



-^ 











\ 







*» 





































л 



\ 









i 









9 



n 











































i- 









i 



































Тещ 



1/. 















Sal 



é 



■inn 





















































200 



300 



МО 



Söo 



station LXXVII. 



rent, and that the latter does not reach further in than to a distance 

 of 6—8 miles from the coast at 76°— 78° N. L. 



At the stations LXXV and LXXVI we find a surface-layer of 

 polar water, which down to a depth of ca. 5 m. is warmed up to over 



