Paper
1 September 1990 Radiative-transfer-based retrieval of reflectance from calibrated radiance imagery measured by an imaging spectrometer for lithological mapping of the Clark Mountains, California
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Abstract
Spectral radiance imagery measured by the Airborne Visibleflnfrared Imaging Spectrometer (AVIRIS) are reduced to reflectance through compensation for atmospheric scattering water vapor absorption absorption of the well mixed gases solar irradiance and the solar zenith angle. The LOWTRAN 7 (Kneizys et al. 1989) radiative transfer code form the basis for this retrieval. LOWTRAN 7 is constrained with water vapor determinations from the AVIRIS radiance data through an algorithm operating on the 940 urn atmospheric water band for every spatial element. In situ measurements of atmospheric optical depths are used to constrain the LOWTRAN 7 aerosol models. Accuracy of the retrieved reflectance spectra is evaluated with respect to surface spectra measured at the time of the overflight. The mineral bastnaesite is identified in the analysis of the retrieved reflectance imagery. These reflectance data provide a means to map the subtle mineral gradients in the PreCambrian block of the Clark Mountain range in southeastern California for geological analysis. 1. 0
© (1990) COPYRIGHT Society of Photo-Optical Instrumentation Engineers (SPIE). Downloading of the abstract is permitted for personal use only.
Robert O. Green "Radiative-transfer-based retrieval of reflectance from calibrated radiance imagery measured by an imaging spectrometer for lithological mapping of the Clark Mountains, California", Proc. SPIE 1298, Imaging Spectroscopy of the Terrestrial Environment, (1 September 1990); https://doi.org/10.1117/12.21353
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Cited by 8 scholarly publications.
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KEYWORDS
Reflectivity

Calibration

Data acquisition

Radiative transfer

Atmospheric modeling

Atmospheric optics

Absorption

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