forward allowance for time changes wliich no doubt resulted from the 

 gale which occurred between the occupation of stations 5734 and 5735. 

 The loss of volume southward, both inside the triangle and between 

 the triangle and the section across the Labrador Sea, is in accord 

 with the reports of exceptional numbers of bergs south-southeastward 

 of Cape Farewell. As suggested above, perhaps even more than the 

 estimated 0.6 moved southward and eastward south of the tiiangle. 

 In considering the temperature sections forming the three sides of 

 the triangle (figs. 27, 29, and 31), it will be noted that the temperature 

 structure in the vicinity of Cape Farewell is markedly different in 



O <T> f^ 0)10 'ij- to 



^ ro ro ro to rO ro 



is» 1^ (^ h- r^ t^ h- 



in if> If) IT) If) lO If) 



31.39 32.5033.18 34.85 34.88 34.73 34.62 



500 



1000 



511500 



UJ 



o 



liJ 



u2000 



2500 



3000- 



GREENLAND 

 K— 50 Ml. 



Figure 32. — Salinity distribution southea.st of Cape Farewell, Greenland, 2-4 



September 1954. 



107 



