HORTON: THE EFFECT OF ROUGH INTERFACES ON SIGNALS 

 THAT PENETRATE THE BOTTOM 



path will depend on the reflection coefficient at the interface and 

 the attenuation the path receives in the sediment. 



REFERENCES 



Brekhovskikh, L. M. , Waves in Layered Media, pp. 117-122, 189-193, 

 Academic Press, 1960. 



Eckart, C. , J. Acoust. Soc. Am. 25, 566, 1953. 



Hamilton, E. L., "Geoacoustic Models of the Sea Floor," in Physics of 

 Sound in Marine Sediments, Ed. Loyd Hampton, Plenum Press, 1974. 



Morris, H. , J. Acoustic Soc. Am. 48, 1198, 1970. 



Pekeris, C. L., J. Acoust. Soc. Am. 18, 295, 1946. 



Urick, R. J., "Underwater Sound Transmission Through the Ocean Floor," 

 in Physics of Sound in Marine Sediments , Ed. Loyd Hampton, Plenum 

 Press, 1974. 



Wood, D. H., J. Acoust. Soc. Am. 46, 1333, 1969. 



294 



