DISCOVERY REPORTS 



unfortunately not fitted to the reversing water bottles used below 400 m. Consequently 

 the isolines below this depth in the vertical sections at this station are situated too low. 



STATION WS382 WS383 W53B4 W5385 

 KING GEORGE I. 3400& 33;30&3370& 



WS386 

 3360S& 



WS387 WS388 

 34-1 0%o_ 



: 3420°4~ 

 "3430&, 



TRINITY PENIN6 



500 



1000 



1500 



2000m 



Fig. 17. Vertical section of salinity: King George Island to Trinity Peninsula, February 1929. 



TRINITY PENIN* 



STATION WS382 W5383 WS384 WS385 



KING GEORGE I. _ _2Q° |5°_ 



ii 



WS38G WS387 WS388 

 10° 



500 



1000 



1500 



2000 M 



Fig. 18. Vertical section of temperature : King George Island to Trinity Peninsula, February 1929. 



Nevertheless the slope of the lines of equal density between Sts. WS 382 and WS 383 

 shows the presence of the north-east going current which sets up the strait on this side. 



