always, Integrating (19) with respect to i fiom 2 to £ p and 
following expression for ee A ) 
yo)= =; & je = */04.) £ x 
ae cosh (PY Jeas(q: Ve) 4 2PR cal Yes Jn oe 
SP Y/a,) po07(@ Sa TRE uh 
equating the real part of the resulting equation to zero, we have the | 
: 
et PS SPA DSL (php, i (7p) +3 Pat 
T ee Ms ca Pee i, 
+ 85h d Dek | 
pa Auhl PI Min oc) 3a . cork (P (P. 2h) oy ‘ 
am pit Psa Ph (P 79, \0ok ( (Bip, area la ea ne | 
oT Dy | (FART ae (Te) Fen a Yo yap. Ad | 
(22) ie 
If we substitute this expression in (12) or 
We 
: fad ar Tian \E AA, 
(23) 
we have the surface slope as induced by the wind stress whose components 
are Tr and 1G respectively. 
Ones the expression for 4 A ) is determined, we can obtain 7/ : 
and VU ‘ty substituting y ( ‘\) in (19). Further substitutions of (4, and 4 
in expressions (10) and (12) will give the horizontal components of velocity. 
The vertical velocity can be er fron 
et x oe (24) 
