B^(p), B^i^) and B^(p) are given by (55), (57), and (80). Let the 

 density of the air he p • = 1.25*10~-^ and the density of the sea 

 water p = 1«028. The other constants, which act in the formulas 

 are already explained and their numerical values are given in the 

 preceding text, K,, K^ and K^ in (82), (83) and (84) are constants 

 of integration, taking into account a duration parameter gt/v as an 

 additional value at the lower limit of integration. 



Case B ; Growth of t h e sea with a constant wind of iinlimited 

 duration as a fu n ction of fetch x . 



1) ^ = ^6.rV "2 _^^li_^_^^p. p<i/3 . (85) 



2) ^ = ^ 2.V J^^ ^c,(pr- il(h"^^ ^P - K,- l/3^p<p^; (86) 



3) ^ = I ^ -' '^^^'' 2 ^ii^^^^ . K^'; 



"" ° Cp(p^)-^6(l)2M(p^)exp[(r/n)(l-8 )6(1)] 



p*V^ m m 



p(l) ; 0<6(l)<6(l)jjj ; (87) 



Pm* 



where K, ', Kp , and K^' are constants of integration. 

 The equations relate 



p or p* = (p(^), and p or p* = F(^) (89) 



V 



for the phase velocity (c = v«p) considering the state of wave 

 development 



either for p^p^^ or for 1^^*^^^* , 



97 



