Effect of Cloud Scattering on Line Formation in the Atmosphere of VenusSource: Journal of the Atmospheric Sciences:;1969:;Volume( 026 ):;issue: 003::page 511Author:Potter, J. F.
DOI: 10.1175/1520-0469(1969)026<0511:EOCSOL>2.0.CO;2Publisher: American Meteorological Society
Abstract: Corrections for anisotropic scattering in a cloudy medium are added to a synthetic spectrum analysis by Belton, Hunten and Goody of CO2 bands and a water vapor line in the spectrum of Venus. It is found that to a good approximation the introduction of anisotropic scattering merely renormalizes the theoretical curves so that the corrections can be applied without recalculating the synthetic spectra. Since the line shapes and relative intensities are unaltered, derived pressures and temperatures remain the same. The corrected results indicate that the scattering mean free path in the Cytherian clouds resembles that for terrestrial cirrus clouds and that there is at least 20 times too little water vapor present to be in equilibrium with a water or ice cloud.
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contributor author | Potter, J. F. | |
date accessioned | 2017-06-09T14:14:52Z | |
date available | 2017-06-09T14:14:52Z | |
date copyright | 1969/05/01 | |
date issued | 1969 | |
identifier issn | 0022-4928 | |
identifier other | ams-15609.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4151300 | |
description abstract | Corrections for anisotropic scattering in a cloudy medium are added to a synthetic spectrum analysis by Belton, Hunten and Goody of CO2 bands and a water vapor line in the spectrum of Venus. It is found that to a good approximation the introduction of anisotropic scattering merely renormalizes the theoretical curves so that the corrections can be applied without recalculating the synthetic spectra. Since the line shapes and relative intensities are unaltered, derived pressures and temperatures remain the same. The corrected results indicate that the scattering mean free path in the Cytherian clouds resembles that for terrestrial cirrus clouds and that there is at least 20 times too little water vapor present to be in equilibrium with a water or ice cloud. | |
publisher | American Meteorological Society | |
title | Effect of Cloud Scattering on Line Formation in the Atmosphere of Venus | |
type | Journal Paper | |
journal volume | 26 | |
journal issue | 3 | |
journal title | Journal of the Atmospheric Sciences | |
identifier doi | 10.1175/1520-0469(1969)026<0511:EOCSOL>2.0.CO;2 | |
journal fristpage | 511 | |
journal lastpage | 517 | |
tree | Journal of the Atmospheric Sciences:;1969:;Volume( 026 ):;issue: 003 | |
contenttype | Fulltext |