1997
DOI: 10.1080/07038992.1997.10855196
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Atmospheric Correction Validation of casi Images Acquired over the Boreas Southern Study Area

Abstract: h~x. T. ox-in • r. Zagobki • \1. Bergeron' \. Roycr > .I. R. \Iiller' .I. I· rccmantle RESUME Des procedures de correction atmospherique a haute altitude d'images de teledetection acquises au moyen du capteur casi (Compact Airborne Spectrographic Imager) dans le cadre du projet BOREAS (Boreal EcosystemAtmosphere Study) ont ete testees au-dessus d'une variete de sites de validation. Une analyse de regression appliquee sur des donnees casi multi-altitudes a ete utilisee pour estimer les facteurs de reflectance … Show more

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Cited by 46 publications
(10 citation statements)
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“…CASI hyperspectral data were processed to surface reflectance using an operational procedure developed at the Earth Observations Laboratory at York University. The processing stream includes conversion of raw data into at-sensor radiance using calibration coefficients determined in the laboratory, surface reflectance retrieval using the CAM5S atmospheric correction model (O'Neill et al, 1997), platform motion removal and image geometric correction using navigation data, and flat field adjustment for residual atmospheric effect removal. Aerosol optical depth at 550 nm, measured with a ground sun-photometer during the airborne data acquisition, was used for atmospheric correction.…”
Section: Remote Sensing Data Pre-processingmentioning
confidence: 99%
“…CASI hyperspectral data were processed to surface reflectance using an operational procedure developed at the Earth Observations Laboratory at York University. The processing stream includes conversion of raw data into at-sensor radiance using calibration coefficients determined in the laboratory, surface reflectance retrieval using the CAM5S atmospheric correction model (O'Neill et al, 1997), platform motion removal and image geometric correction using navigation data, and flat field adjustment for residual atmospheric effect removal. Aerosol optical depth at 550 nm, measured with a ground sun-photometer during the airborne data acquisition, was used for atmospheric correction.…”
Section: Remote Sensing Data Pre-processingmentioning
confidence: 99%
“…Hyperspectral data were processed to atsensor radiance using calibration coefficients derived in the laboratory by the Centre for Research in Earth and Space Technology (CRESTech). Aerosol optical depth at 550 nm was derived from Micro-Tops II sunphotometer (Solar Light, Philadelphia, PA, USA) readings taken in the study area at the time of data acquisition, and subsequently used to process image data to ground-reflectance using the CAM5S atmospheric correction model (O'Neill, Zagolski, Bergeron, Royer, Miller, & Freemantle, 1997. Reflectance data were geo-referenced using GPS data collected onboard the aircraft.…”
Section: Airborne Hyperspectral Data Collectionmentioning
confidence: 99%
“…The 12-bit radiometric resolution data collected by CASI were processed to at-sensor radiance using calibration coefficients derived in the laboratory by the Centre for Research in Earth and Space Technology (CRESTech). Aerosol optical depth data at 340, 380, 440, 500, 670, 870, and 1020 nm were collected using a Micro-Tops III sunphotometer in the study area at the time of data acquisition in order to derive aerosol optical depth at 550 nm to be used to process image data to ground-reflectance using the CAM5S atmospheric correction model [52]. Reflectance data were georeferenced using GPS data collected onboard the aircraft.…”
Section: Methods and Experimental Datamentioning
confidence: 99%