Abstract A widely used algorithm, Sen2Cor, for the atmospheric correction of Sentinel-2 MSI images assumes a constant ratio of red (0.6 μm) and near-infrared (2.2 μm) spectral reflectance, taking ρ 2.2 / ρ 0.6 = 2. In fact, however, this ratio exhibits substantial dependence on vegetation phenology. The discrepancy produces errors in predicted surface reflectance. We analyse the reflectance of 92,230 forest stands, using full time series of Landsat-8/9 OLI and Sentinel-2 MSI images taken over Estonia. We find the ρ 2.2 / ρ 0.6 value for evergreen needleleaf forests to be rather stable over time, with a mean value around 2.25. In broadleaf deciduous forests, on the other hand, we find ρ 2.2 / ρ 0.6 to increase rapidly in the spring, to remain on average close to 3 or greater, and then to decrease in the autumn. We offer parametric and tabulated models of ρ 2.2 / ρ 0.6 for eventual integration with Sen2Cor.
Lang et al. (Mon,) studied this question.