382 



Alf Trolle. 



The salinity in the uppermost 25 m. was somewhat less than 

 at Maroussia, but somewhat greater than further into Stormbugt. 



The temperature was 0.04° above freezing point and the cause 

 of this rise of the temperature above the freezing point temperature 



Tejnp 



Density Z'ioo 11 so 7S 25 oo гь 



Salinity %0 31 DO 26 50 75 3Z 00 25 



era.ture-2° 8 _ t * 2 "Г 



100 



V) 



5 200 



.g 



soo 



й/ту. 



75 Z(j 00 Z5 



?5 33 00 25 



2 J 



T 



27 00 ?5 



so 



75 



28 00 



ЪЧ 00 25 



so 



75 



5Soo 



e i-V 



г 



* 



6 



Sal. 



Лел! 



*Z° 



200 



300 



too 



Station LXI. Lille-Belt. 



was, probably, in part mixing with warmer water from the deeper 



layers, in part mixing with the warmed water from the melting snow 

 and ice, which filtered through the porous ice. 



density ZtOO 25 so 7S 2S0O 25 50 75 26 00 25 SO 75 27,00 25 50 75 28.00 



Salinity %0- 31 00 25 50 75 32 00 25 50 75 ЗЗОО 25 SO 75 5^00 25 50 75 3500 



Temperature. -2°_ a . t » z -V ъ js t z_0 г «6 e »1 ' г t 6 e_jt-2' 



100 



200 



■3 MO 



(=1 



MO 



500 





1^ 











1 — "^ 









\ 























к 

















■Ck.^ 



°— n 



'''* 





















1 





















t 





\ 















^ 



'b 





















\ 





\ 















t) 



'^^ 



Tcmj 



V 

















Sal 





J)CJL 















Ч 









































3 



ä 







































r 



'IS 







































1 



! ^ 













































































100 



zoo 



500 



400 



500 



Station LIX. Stormbugt. 



Series LIX, Stormbugt. 11—13 June 1908. 



The station lay in a small bay, which united the three entrances 

 Store Belt, Lille Belt and Øresund and which received the name of 

 Stormbugt from the German Germania Expedition of 1870 — 71. 



