253 



DEPARTMENT OF THE NAVAL SERVICE 



of inflow be iSet in motion by an anticydonic wind, then the physical process by which 

 the water is introduced is transferred to a greater depth, whereby the Archimedaan 



Y\g. 42 — Current from centre of ])n)duction to cencreof consumptioii in an oceanic layer. 



forces attain a higher degree of intensity, and the current becomes greater. This takes 

 place in thel Gulf Stream, vide fig. 43. 



Fig. 43. — Schematic diagram showing 

 movement of surface water in the 

 Gulf Stream. 



