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Estimating the altitude of aerosol plumes over the ocean from reflectance ratio measurements in the O2 A-band
2009
Remote Sensing of Environment
A methodology is proposed to infer the altitude of aerosol plumes over the ocean from reflectance ratio measurements in the O 2 absorption A-band (759 to 770 nm). The reflectance ratio is defined as the ratio of the reflectance in a first spectral band, strongly attenuated by O 2 absorption, and the reflectance in a second spectral band, minimally attenuated. For a given surface reflectance, simple relations are established between the reflectance ratio and the altitude of an aerosol layer, as
doi:10.1016/j.rse.2009.04.018
fatcat:3plfvqectnau3ixbwevqhmn5se