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Journal ArticleDOI

An introduction to atmospheric radiation

Kuo-Nan Liou, +1 more
- 01 Jul 1981 - 
- Vol. 34, Iss: 7, pp 66-67
TLDR
In this paper, the basic principles of radiative transfer in the Earth's atmosphere are discussed, including thermal infrared radiation transfer and light scattering by atmospheric particulates, and the application of radiative transfer principles to remote sensing.
Abstract
Fundamentals of Radiation for Atmospheric Applications. Solar Radiation at the Top of the Atmosphere. Absorption and Scattering of Solar Radiation in the Atmosphere. Thermal Infrared Radiation Transfer in the Atmosphere. Light Scattering by Atmospheric Particulates. Principles of Radiative Transfer in Planetary Atmospheres. Application of Radiative Transfer Principles to Remote Sensing. Radiation and Climate.

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Citations
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Journal ArticleDOI

Numerically stable algorithm for discrete-ordinate-method radiative transfer in multiple scattering and emitting layered media.

TL;DR: An advanced, thoroughly documented, and quite general purpose discrete ordinate algorithm for time-independent transfer calculations in vertically inhomogeneous, nonisothermal, plane-parallel media for Atmospheric applications ranging from the UV to the radar region of the electromagnetic spectrum is summarized.
Journal ArticleDOI

Narrowband to broadband conversions of land surface albedo I Algorithms

TL;DR: In this paper, the authors applied an approach that decouples surface reflectance spectra from the real-time radiative transfer simulations to calculate the total shortwave albedo, total-, direct-, and diffuse-visible, and near-infrared broadband albedos for several narrowband sensors.
Journal ArticleDOI

Towards Aerosol Light-Absorption Measurements with a 7-Wavelength Aethalometer: Evaluation with a Photoacoustic Instrument and 3-Wavelength Nephelometer

TL;DR: In this paper, a model-based calibration scheme for the 7-wavelength aethalometer was developed to evaluate the filter loading effect caused by aerosol light absorption, and the model is tested against ambient measurements and is found to require coefficients that are situation specific.
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