Aii-101 58 



It would be Interesting to ascertain hov/ vjell our pre- 

 dicted results agree with observation; specifically, if the mass 

 transport of the Gulf Stream responds as indicated to variations 

 in the wind and if the lag of the transport is independent of 

 the frequency, 



5. Methods . of Solution for Prob lem 2. The equations 

 (3« 25) - (3* 30) are non-dimensionalized below in order that 

 boundary layer theory may be employed. Using the arguments of 

 Section h for the method of non-dimensionalizing, we have 



sx 



. _ gW 



^^ , 



ng(D-, - Dp) 

 9 = -i i- 



p2s3 



^ " ?7 ' 



ps-^ 



ps ' 





2 2 

 TT - P ^ P2^2 

 ^2 - —r^ ' 



Then equations (3.25) - (3-30) become 



