and B slope of the water surface was Greet ae devant] distances from ri 
- the coast. Both the surface slopes induced by the offshore and longshore - 
"vind stress components are given in Tables I and II. 
From these results it can be concluded that the slope of the water 
face is chiefly found in the wind zone and it is mostly very small 
side the latter. However, the Tannen of increase of the slope of the 
eer surface with tee ratio ke / Pp is much different between the 
offshore and longshore winise In case of the offshore wind (x the i 
8] pe indueed by it dees not wary much “with the ratio A ie ope > Their 
es within the wind zone lie mostly between | | 
- 
to Ga At iad = 1, the slope varies rather wee g This 
be dangerous to believe this result to be very accurate. At any rate 
=o ee 
4 From this result it can be concluded that the slope of the sea surface 
3 ead by wind stresses is proportional to the wind stress Tz _ and G 
recly to the depth b of the sea provided the ratio By Die asia 
are nearly independent of the smal tele ie or the a turbulence. 
a]J= 
