98 MARION AND GENERAL GREENE EXPEDITIONS 



70 70 60 50 40 3D 



,' M ; / J 



,60 50 



Figure 61. — Salinity at COO meters July 19-September 11. 1928. 



Attention is particularly invited to the position of p. salient formed 

 by both the 4° isothern and the 34.8%o isohaline (figs. 54 and 

 55) off southern Labrador in the vicinity of latitude 55° N., longi- 

 tude 50° W. The distribution of temperature and salinity, corre- 

 sponding to the circulation (fig. 47), indicates a convergence of cool, 

 low-salinity surface layers from the Labrador slope with the inshore 



i 



