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The atmospheric correction of hyperspectral remotely sensed images for the retrieval of biogeochemical variables in
hypertrophic inland waters is an area of ongoing research. We implemented a radiative transfer model (RTM) processing
scheme based on 6S (Second Simulation of the Satellite Signal in the Solar Spectrum) to extrapolate from PRISMA L1 topof-atmosphere radiance data to above-water remote sensing reflectance (Rrs) in a hypertrophic water reservoir located in Valencia, Spain. We obtained a very good agreement
between the in–situ and the atmospherically corrected Rrs (R2 = 0.89, RMSE = 0.0017 sr−1) within the 400–900 nm wavelength range.
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