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Infrared remote soundingAtmospheric 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.
Document ID
19750003490
Acquisition Source
Legacy CDMS
Document Type
Conference Paper
Authors
Rodgers, C. D. (Oxford Univ. Oxford, United Kingdom)
Date Acquired
August 8, 2013
Publication Date
January 1, 1974
Publication Information
Publication: Calif. Univ. Proc. of the UCLA Intern. Conf. on Radiation and Remote Probing of the Atmosphere
Subject Category
Earth Resources And Remote Sensing
Accession Number
75N11562
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.

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IDRelationTitle19750003477Collected WorksProceedings of the UCLA International Conference on Radiation and Remote Probing of the Atmosphere
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