of the North Atlantic eddy entering and leaving the Labrador Sea. 

 There is also an indication of a weak counterclockwise eddy be- 

 tween this water and the West Greenland Current. 



The volume of flow, mean temperature, and heat transport of the 

 Labrador Current past this section has already been presented 



-3ui. 



Figure 21. — Dynamic topography of the sea surface relative to the 1500-decibar 

 surface, from data collected 18-23 July 1951. 



