DAVIS STRAIT AND LABRADOR SEA 

 70 70 3Q 50 40 



93 



60 50 



Figure 56. — Temperature at 200 meters July 19-September 11, 1928. 



warm areas, both of which lay outside of the American slope, are 

 revealed by the surface temperature map (fig. 52) — the one off 

 southern Labrador and the other off middle Labrador. The former, 

 undoubtedly, is a reflection of the Atlantic Current and the latter 

 the result of solar warming in a locality free from active circulation. 



