Velocity profiles have been examined for each of the three sides of 

 the Greenland triangle, and the resulting volume transports for the 

 north, southeast, and southwest sides were 10.49, 0.47, and 8.99, 

 respectively. As these figures indicate about 10 percent greater 

 volume transport into the triangle than that leaving it, the computed 

 volumes have been adjusted to equality for representation in figure 21. 

 The mean temperatures for the sections, in the same order, were 

 5.37, 5.62, and 5.15, resulting in heat transports of 56.28, 2.65, and 

 46.25, respectively. As the point of beginning and ending was at the 

 shallow corner of the triangle, it is difficult to make any straight- 



o (j> (^ CO in 



^ ro ro to ro 



fs. r^ h- r- 1^ 



If) if) lo in If) 



2.50 2.20 8.35 771 



ro 

 in 



8.52 



to 



lO 



in 



8.57 



CVI 



ro 

 in 



10.20 



Figure 31. — Temperature distribution southeast of Cape Farewell, Greenland, 



2-4 September 1954. 



106 



