of 3.2° for the East Greenland Current component and 5.5° for the 

 Inninger Current component, the observed volume transport breaks 

 down into 2.1.3 and 6.82, respectively, for these components, compared 

 with seasonal normal volume transports for these components of 

 0.09 and 4.42. On this basis then, each of the components were 

 about 2 above normal in volume w^ith a resulting heat transport 24.60 

 above normal. In view of the low salinity maximum it is quite 

 possible that more of the West Greenland Current past this section 

 approaches from the south than the 0.1 estimate shown in figure 21. 

 In examining the complete South Wolf Island-Cape Farewell section 

 for volume of flow it was found that, if the velocities are referred to 



ro^ in to 00 o^ 



O — 



OJ OJ 



mm m m m m m m 



32.93 32.67 33.98 34863486 34.71 34.73 



500 



1000 



oIlSOO 



UJ 



o 



Ifiaooo^ 



2500- 



3000- 



GREENLAND 



K-50MI 



Figure 28. — Salinity distribution east of Cape Farewell, Greenland, 29-31 



August 1954. 



342128 — 55- 



103 



