Paolo Colandrea

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Aerosol optical thickness (AOT) values have been retrieved from radiances measured by radiometers and spectrometers such as METEOSAT, AVHRR (Advanced Very High Resolution radiometer), GOES (Geostationary Operational Environmental Satellite) and POLDER (Polarization and Directionality of the Earth’s Reflectance). Early single-band methods are now superseded(More)
The relationship between the normalized radar cross section and the ocean surface wind field, i.e., the geophysical model function, is a key element in scatterometry. Due to many unsolved physical modeling problems, only a semi-empirical approach can be used to quantitatively relate the observed to the wind field. Once the appropriate functional form has(More)
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