128 



Both the northern end of this section and the Davis Strait section 

 show that a part of the Baffin Land Current crossing Davis Strait 

 Ridge extended more than half way across the strait. 



-Dynamic topography of surface relative to 2.000 decibars. 

 August 2, 1938. 



Post-season cruise, July 2i- 



The volume of flow of the various currents crossed has been com- 

 puted and the results are given below in tabular form in comparison 

 with the average of prior investigations given in detail in Bulletin 

 No. 19, part 2 of this series. The volume of flow is given in nnlhon 



