NEAR BOTTOM ENERGY 



(876) 



200 



HIGH FREQUENCY 



SEMIDIURNAL 



INERTIAL 



DIURNAL 



O 

 9} 



q: 



DEPTH (m) 

 STATION 



100 141 295 

 LCA LCU LC8 



560 600 

 LCS LCE 



1275 

 LCH 



Figure 6. Spatial distribution of energy in the near-bottom currents along 

 the axis of Lydonia Canyon. The amount of energy in five frequency bands 

 (high frequency, semidiurnal, inertial, diurnal, and low frequency) changes 

 along the canyon axis, presumably as a result of changes in the density field, 

 bottom slope, and incident energy. 



16 



