NASA NTRS · 19750003490
Infrared remote sounding
Abstract
Atmospheric radiation was measured as a function of wavelength, position, angle, and time. Radiation was determined by temperature, cloud (aerosol), composition, and surface emissivity measurements. The theory of radiative transfer is reviewed, along with retrieval methods. Instruments onboard space probes for infrared remote sounding of planetary atmospheres are also described.
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Rodgers, C. D.. 1974-01-01. Infrared remote sounding. https://ntrs.nasa.gov/citations/19750003490
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