OCEAN TEMPERATURES 



405 



TABLE 14 

 Tabulation of the functions f(z) and 



dz 



Thus it appears that 90 per cent of the upward flux is confined to 

 a coastal belt about 250 miles wide. Finally the stream line equation 

 (188) becomes 



17 *l = C 2 (199) 



_ ,93e- 01 * . 



_ e -?rcos H 1 



for the San Diego region, and the stream lines corresponding to C 2 

 equal 0, 0.1, 0.2, 0.3, 0.4, 0.5, 0.6, 0.7, 0.8, 0.9, and 1.0 are shown in 

 figure 17. 



15 







liOO 



Fig. 17. Traces of theoretical surfaces of flow on a vertical plane perpen- 

 dicular to the coast. The flow included between any two consecutive surfaces 

 is one-tenth of the total amount. 



