

Since 



Wo = U + uV 



we now have the cross-shelf (u) component and longshore 

 (v) component of the surface current: 



U^' 



(T'^u.'vo ^a 



L4 



4^P"f 



1 ^1 S»v>U2©-"l rfemV)V+cosV) 



-ft? '^ \^ g] -««} ^-^v w.) 



24 



