Because B = f(v), M(l) must be a function of v too, if we 



assume B * to be constant at all wind velocities. If M(l) represents 



a function of v only, it has to be determined in such a way that 



there are no contradictions to the relation p = f (v) as determined 



for example, in a previous paper [8]^ 



With 



2r(p * - 1) 



^ In 182.5 - In v^ 



it follows from (59) that 



M(l) = 10"^v^[cm"-'-g sec"-*-] . (6l) 



If numerical values for constants are introduced, and (61) is 

 considered, we get from (57a) 



B2(p) = 2.6.10"3p"^ . (62) 



Thus with (60), B2(p) is represented as a function of p. Since C2(p) 

 according to (28) only is a function of p, the difference C2 - Bg = F(p) 



Equation (60) relates the phase velocity (r = 6 v of fully 

 developed "seas" (B -waves) to the wind velocity (v given in cin/sec), 

 and yields practically the same values for v>2 m/sec as calculated 

 previously [8]. Table 6 shows the values p given by (60) and the 



m 



values 6 as published in [8]. 



Table 6. p = f (v) at different wind velocities 

 given by formula (60) and in an 

 earlier report [8], 



V m/sec 2 4 6 8 10 12 I6 20 24 28 



pjjj(60) 0.48 0.56 0.61 0.66 0.70 0.74 0.81 0.88 0.94 1.00 

 PnjCS] 0.425 0.53 0.60 0.66 0.70 0.74 0.81 0.88 0.94 0.995 



83 



