A MODEL DEVELOPED FOR RADIATIVE TRANSFER IN ATMOSPHERE-SEA SYSTEEM IS APPLIED TO REMOTELY SENSED RADIANCES TO EVALUATE ITS APPLICABILITY IN DETERMINATION OF ATMOSPHERIC TURBIDITY. DATA MEASURED WITH DIFFERENT ATMOSPHERIC TURBIDITY OVER CLEAR SEA WATER, BY A MULTISPECTRAL SCANNER INSTALLED ON AN AIRPLANE, HAVE BEEN USED. COMPARISONS OF AEROSOL OPTICAL THICKNESSES OBTAINED FROM REMOTELY SENSED DATA AND MEASUREMENTS OF ATMOSPHERIC TRANSMITTANCE ARE SHOWN AND DISCUSSED.
MARACCI Giancarlo;
1995-03-15
JRC5277
https://publications.jrc.ec.europa.eu/repository/handle/JRC5277,
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