The first atmospheric aerosol backscatter measurements at the rare isotope CO2 wavelength of 9.1 µm were obtained in the troposphere over the Pacific Ocean in May–June 1990. A distinct aerosol backscatter background mode was found in both hemispheres with modal value ∼10−10 m²kg−1sr−1 (backscatter normalized by air density), remarkably consistent with ground‐based and airborne backscatter climatologies collected at other wavelengths, locations, and times.
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Rothermel et al. (1996) studied this question.
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