pixels 
Figure 6 : Plot of the surface reflectance in channel 3 over sunglint. 
Also reported, comparisons with theoretical computations for several wind speed 
Figures 7: Retrieval of the aerosol optical thickness assuming the wind speed found by channel 3. 
We performed the same procedure with the 4 other scenes. Figure 8 gives the results of the reflectance using a 
wind speed as deduced Figure 6 . Figures 9 show the retrieved reflectances assuming a constant optical thickness 
for each scene. The good agreement between the computations and the measurements shows first the good 
retrieval of the reflectance in channel 3 and water vapor from T 4 and T 5 . It also demonstrates that it is possible 
to retrieve aerosol optical thickness over the sunglint. 
Measurements 
Figure 8 : Comparisons for 5 scenes between retrieved reflectance 
and computation using the wind speed. 
Figure 9: Comparisons for 5 scenes between measured and computed reflectance 
assuming a constant aerosol optical thickness and wind speed for each scene. 
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