indicated in Fig. 14 by a broken line. But if the original values 

 of C and B (full lines) were used, the results would not be changed 

 essentially for larger "fetch parameters" or "duration parameters" 

 (see section 7)» The reason for this is that the earliest stages 

 of sea development are so rapid in the state p<l/3, that the rela- 

 tively short fetches (or durations) are of very little consequence 

 to the later development of the sea. Table 5 gives the values of 

 C,(p), C^i^) and B,(p), B2(p) as they are used for the numerical 

 computation. The original values are given in parenthesis, if they 

 differ from the used values. 



Table 5» Values of 'Vesistance-factors" C(p) and 



"dissipation-factors" B(p) for different 

 values of p in the stages p^l.O. 



p 0.05 0.15 0.25 0.30 0.40 0.45 0.55 0.65 0.75 0.85 0.95 1.00 

 C, (p) 16.7513.38 10.65 9.48 



•J-]^q3 (10.42)(9.06) 



C2(p) 7.50 6.71 5.39 4.42 3.71 3.21 2.88 2.78 



.10^ (8.58)(7.30)(5.50) 



^l^^^QP "TO) ^0-2^ 8.60 7.85 

 VP^ (6.38^^5.75^ 4,73 4,01 3.47 3.06 2.75 2.60 



The very rapid development of the sea in the earliest stages at 

 3<l/3 may be shown by an example for a wind velocity v = I6 m/sec. 



The results given in section 7 demonstrate that the state p = I/3 

 is attained from a fetch of only 8.3 km. But a fetch of 300 km is nece- 

 ssary to attain the state p = O.8I = p . That means that at any rate 

 300 km is necessary for the development of the sea to the stage 



81 



