2006
DOI: 10.1080/01431160500486690
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Abstract: The automatic correction of atmospheric effects currently requires visible to short-wave spectral bands (400-2500nm) to derive high accuracy surface reflectance data. Common techniques employ spectral correlations of dark targets in the short-wave infrared (SWIR, around 2.2 mm), blue (480 nm) and red (660 nm) regions to derive the aerosol optical depth. A large number of current Earth-observing satellite sensors have only three or four spectral channels in the visible and near-infrared (VNIR) region (400-1000n… Show more

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Cited by 117 publications
(78 citation statements)
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“…Clouds and cloud shadows, as well as water were masked using the Fmask algorithm [45]. The ATCOR-2 algorithm was implemented [46] to correct for atmospheric and topographic effects, and to derive ground reflectance and surface temperature values from the multispectral and thermal bands, respectively, followed by production of mosaics of the image pairs using PCI Orthoengine.…”
Section: Landsatmentioning
confidence: 99%
“…Clouds and cloud shadows, as well as water were masked using the Fmask algorithm [45]. The ATCOR-2 algorithm was implemented [46] to correct for atmospheric and topographic effects, and to derive ground reflectance and surface temperature values from the multispectral and thermal bands, respectively, followed by production of mosaics of the image pairs using PCI Orthoengine.…”
Section: Landsatmentioning
confidence: 99%
“…For this purpose, column water vapor value equals 2.0 g cm −2 are used and the sensor altitude is approximately 5 km above sea level resulting in pixel size of 4 m. To obtain a realistic range of AOD for the forward modeling, the method of [25] was applied on three real APEX sensor [45] radiance cubes of the Coast of Belgium. The reason for using the coastal area is its diversity, as the scene is covered by both sea and land.…”
Section: Profile Of the Condition Parameters For The Usual Scatteringmentioning
confidence: 99%
“…Estimating a range of AOD is not straightforward with the method of [25] as it provides visibility (in km) as an output. In MODTRAN 4, both AOD and visibility are used to describe the aerosol optical properties.…”
Section: Profile Of the Condition Parameters For The Usual Scatteringmentioning
confidence: 99%
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