2014
DOI: 10.1016/j.rse.2014.08.001
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On-orbit radiometric characterization of OLI (Landsat-8) for applications in aquatic remote sensing

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Cited by 200 publications
(117 citation statements)
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“…In particular, S2A TOA radiances were computed from the S2A-MSI level2 TOA reflectance images (downloaded from Copernicus Open Access Hub) by using the SNAP tool ReflectanceToRadianceOp. For L8-OLI, (downloaded from U.S. Geological Survey EarthExplorer portal) the level1B products were converted into TOA radiances by applying radiometric calibration gains and then rescaled using aquaticspecific gains (Pahlevan et al, 2014). Both S2A and L8 TOA radiance products were atmospherically corrected through an algorithm based on the vector version (6SV) of Second Simulation of the Satellite Signal in the Solar Spectrum (Vermote et al, 2006).…”
Section: Image Processingmentioning
confidence: 99%
See 1 more Smart Citation
“…In particular, S2A TOA radiances were computed from the S2A-MSI level2 TOA reflectance images (downloaded from Copernicus Open Access Hub) by using the SNAP tool ReflectanceToRadianceOp. For L8-OLI, (downloaded from U.S. Geological Survey EarthExplorer portal) the level1B products were converted into TOA radiances by applying radiometric calibration gains and then rescaled using aquaticspecific gains (Pahlevan et al, 2014). Both S2A and L8 TOA radiance products were atmospherically corrected through an algorithm based on the vector version (6SV) of Second Simulation of the Satellite Signal in the Solar Spectrum (Vermote et al, 2006).…”
Section: Image Processingmentioning
confidence: 99%
“…Differently from ocean colour satellites, they have not been specifically designed for observing water but they are both promising for detailed water quality analysis (Kutser, 2004;Pahlevan et al, 2014) due to (i) radiometric sensitivity ([ 12-bit quantization) (Hedley et al, 2012;; (ii) spatial resolution of 10-30 m; (iii) frequency of overpass (up to every 2-3 days combining L8 and S2 satellites); and (iv) the improved spectral band configuration in the visible-near-infrared wavelengths range.…”
Section: Introductionmentioning
confidence: 99%
“…The algorithm (version 2016.05.20) allows the user to choose some inputs for the atmospheric correction: (i) derive ε fixe on scene, per pixel or user-defined; (ii) gain factors for radiometric calibration [56,57]; (iii) atmospheric pressure; (iv) smooth window applied to aerosol reflectance values; and (v) cloud mask threshold (default: 0.0215 on the 1610 nm band). In our study, atmospheric correction was performed using the SWIR band approach, as recommended for turbid water [55]; aerosol correction per-pixel; a smooth window of 25 pixels; and cloud dilatation of 16 pixels (default).…”
Section: Acolite Algorithmmentioning
confidence: 99%
“…The RSR curves in the visible and NIR bands are shown as dashed lines in Figure 2. Although L8/OLI is not designed for ocean monitoring, its advantages of high spatial resolution and the increased number of bands, combined with its improved signal-tonoise ratio and data quality, make it increasingly used in ocean color remote sensing research and especially in estuarine and coastal research [26][27][28][29][30][31][32][33].…”
Section: Satellite Imagesmentioning
confidence: 99%