Table 2. 



Limit for validity of cnoidal 

 theory for normal incidence. 



s 



"o 

 L 







\ 

 ^ 



.01 



.046 



0.385 



.02 



.076 



0.576 



.03 



.107 



0.741 



.04 



.139 



0.872 



.05 



.173 



0.993 



10 20 30 40 50 60 70 80 90 



Figure 13. Wave breaking angle, a.]-,, as a function of 

 deepwater wave angle, a^, and deepwater 

 steepness, H^/L^, on a bottom slope, S = 0.01. 



32 



