L8/OLI Rrsderived using the (a) M6SV, (b) VR-SWIR-F, and (c) SD-SWIR models plotted against in situ measurements from Taihu Lake at 13 synchropoints. The solid line is a 1:1 line; the dashed lines represent ± 15% error around the 1:1 line. The mean ratio (MR) represents the ratio between the model-derived Rrs and in situ-measured Rrs for each band. (d) A comparison of the mean Rrs spectra from the three models and the in situ measurements at the 13 synchropoints.</p
CHRIS (Compact High Resolution Imaging Spectrometer) is an exploring hyperspectral remote sensor, ca...
The standard SeaWiFS atmospheric correction algorithm, designed for open ocean water, has been exten...
[Departement_IRSTEA]Eaux [TR1_IRSTEA]QUASARE [ADD1_IRSTEA]Systèmes aquatiques soumis à des pressions...
(a-c) Examples of validation comparisons between model-derived Rrsand in situ measurements from Taih...
Rrs(λ) density-sliced scatterplots at wavelengths of (a) 483, (b) 561, (c) 655, and (d) 865 nm. The ...
During the atmospheric correction of remote sensing data in inland waters, the original Second Simul...
Results for the atmospheric correction of an L8/OLI image (Taihu Lake, China, October 26, 2014) usin...
The OLI (Operational Land Imager) sensor on Landsat-8 has the potential to meet the requirements of ...
The Operational Land Imager (OLI) onboard Landsat 8 is generating high-quality aquatic science produ...
The optimal exploitation of the oceanic information provided by recent high spatial resolution senso...
A common approach to the pixel-by-pixel atmospheric correction of satellite water colour imagery is ...
AbstractMonitoring of water quality by satellite ocean colour data requires high quality atmospheric...
A three-component reflectance model (3C) is applied to above-water radiometric measurements to deriv...
Atmospheric correction (AC) is the basis for quantitative water remote sensing, and adjacency effect...
Although designed for land surfaces, MODIS Aqua surface reflectance data products (MYD09, termed as ...
CHRIS (Compact High Resolution Imaging Spectrometer) is an exploring hyperspectral remote sensor, ca...
The standard SeaWiFS atmospheric correction algorithm, designed for open ocean water, has been exten...
[Departement_IRSTEA]Eaux [TR1_IRSTEA]QUASARE [ADD1_IRSTEA]Systèmes aquatiques soumis à des pressions...
(a-c) Examples of validation comparisons between model-derived Rrsand in situ measurements from Taih...
Rrs(λ) density-sliced scatterplots at wavelengths of (a) 483, (b) 561, (c) 655, and (d) 865 nm. The ...
During the atmospheric correction of remote sensing data in inland waters, the original Second Simul...
Results for the atmospheric correction of an L8/OLI image (Taihu Lake, China, October 26, 2014) usin...
The OLI (Operational Land Imager) sensor on Landsat-8 has the potential to meet the requirements of ...
The Operational Land Imager (OLI) onboard Landsat 8 is generating high-quality aquatic science produ...
The optimal exploitation of the oceanic information provided by recent high spatial resolution senso...
A common approach to the pixel-by-pixel atmospheric correction of satellite water colour imagery is ...
AbstractMonitoring of water quality by satellite ocean colour data requires high quality atmospheric...
A three-component reflectance model (3C) is applied to above-water radiometric measurements to deriv...
Atmospheric correction (AC) is the basis for quantitative water remote sensing, and adjacency effect...
Although designed for land surfaces, MODIS Aqua surface reflectance data products (MYD09, termed as ...
CHRIS (Compact High Resolution Imaging Spectrometer) is an exploring hyperspectral remote sensor, ca...
The standard SeaWiFS atmospheric correction algorithm, designed for open ocean water, has been exten...
[Departement_IRSTEA]Eaux [TR1_IRSTEA]QUASARE [ADD1_IRSTEA]Systèmes aquatiques soumis à des pressions...