60 



MARION AND GENERAL GREENE EXPEDITIONS 



<\J fO Tj- in to 1^ 

 O O O OO O 



ro ro ro ro to K) 



34.44 3467 3461 



-34.8 

 34a 



34.95 



3491 



3489 



34.89 



30 60 (miles) 



34.63 



B, 



3494 



34.92 



34.91 



Figure 33. 



-Salinity profiles across the continental shelf, Ai, August 1-2, 1931 ; Bi, 

 July 28, 1981 



cordingly, the tongue of coldest water along the southwest coast of 

 Greenland shown by our observations, even if positive in tempera- 

 ture (see fig. 15), has been considered by us as representing the East 

 Greenland Current, and, if so defined, it cannot be said to disappear 

 from the west coast. According to this view east (Treenland Arctic 

 water suffers major diminution near Fylla Bank, and, while there is 



