Paper
14 December 1998 Effect of cirrus clouds in the infrared (4 to 100 μm): high-spectral-resolution simulations
Jaqueline E. Russell, Richard J. Bantges, Catherine Naud, Joanna D. Haigh
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Abstract
The effect of cirrus clouds in the IR has been simulated at high spectral resolution and the sensitivity to crystal, size, aspect ratio, size distribution and cloud ice water path, has been investigated. The single scattering parameters of the cloud particles were determined using Mie theory for distributions of spheres and the T-Matrix method for spheroids. Cloudy-sky radiances, fluxes and atmospheric heating rates were calculated using the discrete ordinates multiple scattering code, with clear sky atmospheric transmission determined using the GENLN2 line-by-line code. It can be seen from these results that both the volume and the cross section of the cirrus particles are important in determining the spectral variation of the radiance and fluxes and also affect their spectrally integrated values. This implies that particle aspect ratio is a radiatively important parameter in the IR. In order to further investigate these differences, singular value decomposition analysis was carried out on seventy spectra calculated for the 700-2500 cm-1 spectral region using spheroids of different size and aspect ratio for a range of cloud ice water paths.
© (1998) COPYRIGHT Society of Photo-Optical Instrumentation Engineers (SPIE). Downloading of the abstract is permitted for personal use only.
Jaqueline E. Russell, Richard J. Bantges, Catherine Naud, and Joanna D. Haigh "Effect of cirrus clouds in the infrared (4 to 100 μm): high-spectral-resolution simulations", Proc. SPIE 3495, Satellite Remote Sensing of Clouds and the Atmosphere III, (14 December 1998); https://doi.org/10.1117/12.332674
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Cited by 2 scholarly publications.
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KEYWORDS
Clouds

Particles

Optical spheres

Atmospheric particles

Infrared radiation

Crystals

Absorption

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