2016
DOI: 10.1016/j.rse.2016.08.010
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CPBAC: A quick atmospheric correction method using the topographic information

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Cited by 15 publications
(9 citation statements)
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“…Satellite remote sensed data are easily influenced by water vapor, aerosol, bidirectional reflection, and data transmission, which will result in serious fluctuations of time series data and influence the desired effect in data analysis [50,51]. Therefore, this study applied the Fast line-of-Sight Atmospheric Analysis of Spectral Hypercubes (FLAASH) [52][53][54] to eliminate such atmospheric interference in each image. A digital elevation model (DEM) [55,56] was used to make terrain corrections, as terrain factors may affect the brightness values of original imagery.…”
Section: Processing Landsat Times Series Productsmentioning
confidence: 99%
“…Satellite remote sensed data are easily influenced by water vapor, aerosol, bidirectional reflection, and data transmission, which will result in serious fluctuations of time series data and influence the desired effect in data analysis [50,51]. Therefore, this study applied the Fast line-of-Sight Atmospheric Analysis of Spectral Hypercubes (FLAASH) [52][53][54] to eliminate such atmospheric interference in each image. A digital elevation model (DEM) [55,56] was used to make terrain corrections, as terrain factors may affect the brightness values of original imagery.…”
Section: Processing Landsat Times Series Productsmentioning
confidence: 99%
“…All the methods can be classified basically into two categories, namely scene-based empirical method and the radiative transfer modeling approach [19,23]. The scene-based methods mainly include the flat field correction method [24], the dark object subtraction [25,26], the empirical line method [27], the internal average reflectance method [28], the cloud shadow method [29], the log residuals calibration [30], and the quick atmospheric correction [31].…”
Section: Introductionmentioning
confidence: 99%
“…The second category comprises atmospheric correction based on the theory of radiative transfer, which establishes the strict radiative transfer model about the radiation transmission process in the range of the visible to short-wave infrared band from the sun to the surface and then to the sensor, and it describes the condition of the radiation source, the atmosphere status, the relationship between the reflection characteristics of the ground objects, and the radiances recorded by the sensor. The atmospheric correction is then conducted on the image by using the measured, or standardized, atmospheric parameters [19,23]. Some typical methods of this category are 6S (Second Simulation of the Satellite Signal in the Solar Spectrum), FLAASH (Fast Line-of-sight Atmospheric Analysis Spectral Hypercubes), ATCOR (ATmospheric CORection), HATCH (High-accuracy Atmospheric Correction for Hyperspectral Data), and BRDF (Bidirectional Reflectance Distribution Function) [23].…”
Section: Introductionmentioning
confidence: 99%
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