Numerical Experiment of Combined Infrared and Ultraviolet Radiation Remote Sensing to Determine the Profile and Total Content of Atmospheric Ozone

Cheng Minghu; Shi Guangyu; Zhou Xiuji

doi:10.1007/BF03179763

Impact Factor: 5.8

Volume 7 Issue 3

Jul. 1990

Article Contents

Article > ADVANCES IN ATMOSPHERIC SCIENCES > 1990 > 7(3): 305-319

Numerical Experiment of Combined Infrared and Ultraviolet Radiation Remote Sensing to Determine the Profile and Total Content of Atmospheric Ozone

1.
Institute of Atmospheric Physics, Academia Siniea, Beijing 100011,Institute of Atmospheric Physics, Academia Siniea, Beijing 100011,Academy of Meteorological Science, State Meteorological Administration, Beijing 100081

doi: 10.1007/BF03179763

Abstract
References
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Abstract:
A new remote sensing method is described to determine the vertical distribution and total content of atmospheric ozone. The method combines surface infrared, satellite infrared and ultraviolet channels. The width of the infrared channels is 0.01 cm-1, less than Lorentz half-width at the earth’s surface, rather than the present width, because these channels can obtain information about variations in the ozone profile below the profile main-peak. The numerical experiments show that the method has a satisfactory precision in determining total ozone content, just about 1 percent error, and vertical distribution from the earth to 65 km space. In addition, some semi-analysis functions for calculating backscattered ultraviolet and a relaxation equation are described in this paper.
References

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Manuscript History

Manuscript received: 10 July 1990

Manuscript revised: 10 July 1990

通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

Numerical Experiment of Combined Infrared and Ultraviolet Radiation Remote Sensing to Determine the Profile and Total Content of Atmospheric Ozone

1. Institute of Atmospheric Physics, Academia Siniea, Beijing 100011,Institute of Atmospheric Physics, Academia Siniea, Beijing 100011,Academy of Meteorological Science, State Meteorological Administration, Beijing 100081

Manuscript received: 1990-07-10
Manuscript revised: 1990-07-10

Abstract: A new remote sensing method is described to determine the vertical distribution and total content of atmospheric ozone. The method combines surface infrared, satellite infrared and ultraviolet channels. The width of the infrared channels is 0.01 cm-1, less than Lorentz half-width at the earth’s surface, rather than the present width, because these channels can obtain information about variations in the ozone profile below the profile main-peak. The numerical experiments show that the method has a satisfactory precision in determining total ozone content, just about 1 percent error, and vertical distribution from the earth to 65 km space. In addition, some semi-analysis functions for calculating backscattered ultraviolet and a relaxation equation are described in this paper.