UNCLASSIFIED 



Jli.CUW1TY CLASSIFICATION OF THIS PAGEITWmi Dmtm Enttnd) 



motions at the local inertial frequencies and the semidiurnal tidal 

 frequency. Spectral analysis indicates that tidal frequency motion is 

 essentially due to baroclinic internal tides and not barotropic surface 

 tides. 



UNCLASSIFIED 



SECURITY CLASSIFICATION OF THIS PAGE(1Wi»n Data BnUnd) 



