Accession Number : AD0764295
Title : On Small Scale Breaking Waves.
Descriptive Note : Technical rept.,
Corporate Author : JOHNS HOPKINS UNIV BALTIMORE MD CHESAPEAKE BAY INST
Personal Author(s) : Banner,M. L. ; Phillips,O. M.
Report Date : JUL 1973
Pagination or Media Count : 31
Abstract : It is shown that the surface wind drift in the ocean substantially reduces the maximum wave height and wave orbital velocity that can be attained before breaking. Incipient breaking is characterized by the occurrence of stagnation points at wave crests, but not by discontinuities in slope. After breaking, there is in the mean flow a stagnation point relative to the wave profile near the crest of the broken wave, on one side of which the water tumbles forward and behind which it recedes more smoothly to the rear. Flow visualization studies indicate the general extent of the wake behind the breaking region; it is shown to be turbulent but momentumless. (Author)
Descriptors : (*OCEAN WAVES, HYDRODYNAMICS), FLOW VISUALIZATION, EQUATIONS OF MOTION, WIND
Subject Categories : Physical and Dynamic Oceanography
Distribution Statement : APPROVED FOR PUBLIC RELEASE