ABSTRACT 



Graphs are presented shewing the max^jntwi speeds 

 -and lengths of bottom oscillations cjie to surfaoe waves as 

 a function of depth for each month (except 

 Beach;. Martha's Vineyard, The ca?.3u'.atlone av°. be,; 



O 1. ■■: 



South 

 d on 



the theory of waves of small 

 sent oscillations due to the 

 waves. 



amp .',\ tilde, 'Jne 

 averago monthly 



data reprec- 

 Bignnf l'';ar-.t 



-1- 



