93 



49° 48° 47' 



52" 51° 50° 49' 48° 47° 46° 45° 44° 43° 



Figure 19. Dynamic current map, from data collected April 10-20, 1935. 



less than it was in April. The comparative weakness of the Labrador 

 Current in latitude 47° N. was correlated at the time with the increas- 

 ing proportion of ice following the Polar Current along the Avalon 

 Peninsula as an indication of a change in the relative strengths of the 

 two branches of the Labrador Current in the vicinity of then- dividing 



