] remote 
the rela- 
orementi- 
in the 
than 
vortices 
e tidal 
11 scale 
ss of the 
the tidal 
1 and in 
ital 
sition 
» 3L and 
‘ound to be 
cess of 
in under- 
is that 
ı beyond 
e Harima 
| observa- 
an be 
ory. In 
2 hour 
  
  
    
    
  
      
Fig. 9. 
HARIMA SEA 
KII CHANNEL 
  
Shikoku 
  
0 5 km 
ll 
Fig. 10. 
741 
ee wn ie 
— Óe A nas 
TIDAL VELOCITY 
(M) (09:48 AUG 01, 1976) 
(3) (09:57 DEC 30, 1975) 
Landsat MSS imageries of the large scale water mass. 
(northward flow) 
D 
  
TIME (hour) 
© 
(southward flow) 
  
Formation process of the large scale water mass. 
ea tr rar na ES