values from the same stations at constant level were plotted (at 

 75 meters off South Wolf Island and at 100 meters for the Bona- 

 vista triangle) this plot showed similarly negative results as to 

 any consistent trend. 



Referring again to table 1 it will be noted that the volume 

 transport of the Labrador Current at the South Wolf Island 

 section was 4.18 whereas that at the Bonavista triangle a few 

 days earlier was 4.98. Usually there is some loss of volume trans- 

 port to the eastward between the South Wolf Island section and 



Table 2 



the Bonavista triangle. With the volume transport some 0.8 higher 

 at the Bonavista triangle than at South Wolf Island the explana- 

 tion would seem to be that at least 0.8 were involved in a cyclonic 

 closed eddy northeastward of the Bonavista triangle. This has 

 been indicated in figure 19 which schematically presents the vol- 

 ume transports listed in table 1. 



52 



