Full text: Actes du Symposium International de la Commission VII de la Société Internationale de Photogrammétrie et Télédétection (Volume 2)

    
  
     
  
  
   
    
  
  
  
   
   
  
     
   
   
   
  
  
  
  
  
   
    
    
   
  
  
  
     
    
    
       
      
  
  
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"vered Fig.l. Dependence of the brightness of sea surface on the solar 
less zenith angle ( 95) and on the wind velocity (W )for the zenith 
Be angle of the observation Im = 2 and at wavelength A =0.7 
on the microns. Continuous lines - for pure water,dotted lines - for 50 
microns thick oil film on the water. The wind and solar azimuth 
= on angles are equal. The Be values are in relative units, the 
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