Retrieval of stratospheric aerosol size distribution from atmospheric extinction of solar radiation at two wavelengths.

The possibility of retrieving size distribution of aerosol particles in the stratosphere by measuring the extinction of solar radiation traversing the aerosol medium at two different wavelengths is explored in this work. This paper presents a parametric study of the effects of size distribution and composition of stratospheric on the value R, the ratio of extinction of solar radiation at wavelength 0.45 μm to the extinction at aerosols wavelength 1.0 μm. The aerosol size distributions under study are nine analytical expressions including most stratospheric aerosol models used by investigators. The aerosol compositions under study are the supercooled sulfuric-acid droplets, with different weight percentages of H2SO4 in the aerosol. It is found that R is not very sensitive to either the composition or the radii limits of stratospheric aerosols under consideration but is quite sensitive to the value of the variable parameter governing the mode radius of the size distribution of aerosol particles. Based on the results of this parametric study, a method of retrieving the size distribution of aerosol particles in the stratosphere from the experimental results of the extinction of solar radiation at two wavelengths is proposed.

[1]  N. Farlow,et al.  Latitudinal variations of stratospheric aerosols , 1979 .

[2]  G. Fiocco,et al.  Sensitivity of the photodissociation of NO2, NO3, HNO3 and H2O2 to the solar radiation diffused by the ground and by atmospheric particles , 1979 .

[3]  R. Turco,et al.  Stratospheric aerosols: Observation and theory , 1982 .

[4]  William P. Chu,et al.  Satellite and Correlative Measurements of the Stratospheric Aerosol. I: An Optical Model for Data Conversions , 1981 .

[5]  M. McCormick,et al.  Satellite studies of the stratospheric aerosol , 1979 .

[6]  M. P. McCormick,et al.  Post-volcanic stratospheric aerosol decay as measured by lidar , 1978 .

[7]  G. Kent,et al.  Atmospheric Backscatter Model Development for CO Sub 2 Wavelengths , 1982 .

[8]  M. Box,et al.  Retrieval of aerosol size distributions by inversion of simulated aureole data in the presence of multiple scattering. , 1979, Applied Optics.

[9]  K. F. Palmer,et al.  Optical constants of sulfuric Acid; application to the clouds of venus? , 1975, Applied optics.

[10]  D. Hofmann,et al.  Balloon‐borne observations of stratospheric aerosol and condensation nuclei during the year following the Mt. St. Helens eruption , 1982 .

[11]  A. Deepak,et al.  Representation of Aerosol Size Distribution Data by Analytic Models , 1982 .

[12]  G. Fiocco,et al.  Effects of radiation scattered by aerosols on the photodissociation of ozone , 1978 .

[13]  Effects,et al.  Atmospheric aerosols : their formation, optical properties, and effects , 1982 .

[14]  M. McCormick,et al.  Inversion of stratospheric aerosol and gaseous constituents from spacecraft solar extinction data in the 0.38-1.0-microm wavelength region. , 1979, Applied optics.

[15]  A. Lazrus,et al.  Measurements of stratospheric sulfate mixing ratio with a multi filter sampler , 1981 .

[16]  Effects of aerosol optical properties and size distributions on heating rates induced by stratospheric aerosols , 1978 .

[17]  R. S. Longhurst Geometrical and Physical Optics , 1967 .

[18]  D. Hofmann,et al.  On the background stratospheric aerosol layer , 1981 .

[19]  Owen B. Toon,et al.  Microphysical Processes Affecting Stratospheric Aerosol Particles , 1977 .

[20]  G. Grams In‐situ measurements of scattering phase functions of stratospheric aerosol particles in Alaska during July 1979 , 1981 .