The radiometric sensitivity of the POLarization and Directionality of the E
arth's Reflectances (POLDER) instrument in the ocean color spectral bands (
443, 490, and 565 nm) was checked vicariously by comparing top-of-atmospher
e normalized radiances measured by the instrument with those computed for t
he same geometries using a radiative transfer model. In situ measurements o
f aerosol optical thickness and marine reflectance at the time of the satel
lite overpass were used as input to the model. The accuracy of the vicariou
s calibration coefficients was estimated to better than 3%, A large decreas
e in the POLDER instrument response was found in the blue, confirming the r
esults previously obtained using alternative techniques.