Pacific Ocean Circulation — • Hid AKA 
201 
where 
ai 
f cos (w. v ) dv 
1 
/ TTZ 
. 2 4 
/ TTZ ' 
\ Sm \2D Z 
\2D Z . 
) 
m 
2 H 
.2 h 
V COS (g- ,) 
dii 
1 
/ xz 
vif; * 
2A ) sin ( 2 S • 2 * 
) + COS 
(ft • “) 
- 1 
/ TTZ ' 
\2D Zt 
)■ 
/ TTZ 
\2Dl ‘ 
2A) 
,'f? 'i 
J- / 
2 h 2 1 
r»2h 
7] 2 COS ^ 
' XZ 
^ 77 
) 
1 
/ jrz_ 
\2D t 
- . 2fc) 
5 / 
/ TTZ 
cos ( 2 ZC • 
2fe) + j 
(ft ■ “) 
- 2 ! 
Si" (Jg- . 2h 
I TTZ " 
\ ' 
/ xz 
. 2/e) 2 
\2D Z , 
) 
\2f; 
( 86 ) 
For larger values of rj, we may express F(rj) in the form 
p ( \ p j fi+i — F-i ( \ | F + i — 2 Fq + F_i , \ 2 
F(^) = F 0 H ^ (’l “ w H 2p “ w 
where F_i, F 0 , and F + i are the values of F(rj) for 7] 0 — h, tj 0 , and tjq + h, respectivelv. 
We have then 
/ % -\-h 
F(rj) cos = ( — ^2 + o) F_i + ($2 — 2 ^ 2 ) F 0 + (&2 + o) F+i 1871 
n 0 ~h 
where 
a2 = l 1 “KS- *)’! “KS*) • 2h ’ 
h = h ) ~ * (S • *)*! sin (£ ’'») h ’ 
Ci = *)1 cos (S ” 0 ) • *• 
( 88 ) 
The integration was carried out taking h = 0.1 in the interval 0 ^ rj ^ 1.0 and h = 1 
for the interval 1.0 S V ^ 10.0. For larger values of tp integration was carried out by 
using formula (82) which is only inversely proportional to nf. In this case, we have only 
to evaluate the integral: 
/ TTZ \ 
1 
