Figure 35. — Siilinity (listril)utioii aloiiK niciididiKil scc-tit)ii at 50°15' W., from 

 dain collected 7-10 April I'.MH). 



Ii-aiisport iiicliidcd this rddy as well as li. Tlic vohiinc Ifaiisport of 

 I lie eddy, estimated as the iicl tiaiispoft hctwccii stations 7oOO and 

 7'M)\, was tluTofofc subtracted to derive li. 



♦.Vpplyins mcnin B for 1938, 1958 and 19(50 to E4-C+B for 1950. 



As lli(> sum of I-'] |)liis (' is one of I he most im[)ortant values which 

 can he derived IVom the occupation (»!' the section, ati extraordinaiw 

 and otherwise imjustifiable procecUire w as followed to get a gross ap- 



56 



