To assess the suspended and dissolved matter in water in the visible and near infrared spectral regions it is necessary to estimate with adequate accuracy the water leaving radiance. Consequently radiance measured by a remote sensor has to be corrected from the atmospheric and the sea surface effects consisting in the path radiance and the sun and sky glitter radiance contributions. T... https://balboasurfandsstylers.shop/product-category/scrunchies/
Correction of sun glint effect on MIVIS data of the Sicily campaign in July 2000
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