HYDROLOGY OF THE BRANSFIELD STRAIT 



15 



is needed to account for the shape the lines of equal density assumed in April 

 1927. 



STATION 196 



K.GEORGE I. 



TRINITY PENIN* 



500 



1000m- 



1500 



2000 



Fig. 9. Vertical section of temperature: King George Island to Trinity Peninsula, April 1927. 



STATION 196 



K.GEORGE I. 27 20 



197 



198 199 



27302240 



200 



2750 



TRINITY PENIN6 



500m- 



1000 



1500m 



EDOOi 



Fig. 10. Vertical section of density (o- 4 ): King George Island to Trinity Peninsula, April 1927. 



The vertical temperature section shows the cold water at all depths at the north-east 

 end of the strait and the slight trace of the warm deep water only at St. 196 closest to 

 King George Island. The vertical salinity section shows the lower saline water below 



