On the satellite retrieval of Saharan dust optical thickness over land: Two different approaches

Two approaches are presented to retrieve the desert aerosol optical thickness over land from satellite. One approach uses the infrared imagery, and the other uses contrast reduction in visible imagery. The retrieved aerosol optical thicknesses from Meteosat data are shown in good agreement with simultaneous ground-based measurements. Advantages as well as deficiencies of both methods are compared.

[1]  Didier Tanré,et al.  Estimation of Saharan aerosol optical thickness from blurring effects in thematic mapper data , 1988 .

[2]  Y. Kaufman,et al.  Field Experiment for Measurement of the Radiative Characteristics of a Hazy Atmosphere , 1986 .

[3]  Michel Desbois,et al.  Satellite Detection of Saharan Dust: Optimized Imaging during Nighttime , 1988 .

[4]  G. d’Almeida,et al.  On the variability of desert aerosol radiative characteristics , 1987 .

[5]  D. Diner,et al.  Atmospheric transfer of radiation above an inhomogeneous non-Lambertian reflective ground—I. Theory , 1984 .

[6]  J. Coakley,et al.  Response of the NCAR Community Climate Model to the Radiative Forcing by the Naturally Occurring Tropospheric Aerosol , 1985 .

[7]  David A. Santek,et al.  A model for calculating desert aerosol turbidity over the oceans from geostationary satellite data. , 1980 .

[8]  M. Griggs,et al.  Satellite Observations of Atmospheric Aerosols During the E0MET Cruise , 1979 .

[9]  Yoram J. Kaufman,et al.  Atmospheric effect on classification of finite fields , 1984 .

[10]  Didier Tanré,et al.  Saharan Aerosols over the South of France: Characterization Derived from Satellite Data and Ground Based Measurements , 1988 .

[11]  P. Deschamps,et al.  Influence of the background contribution upon space measurements of ground reflectance. , 1981, Applied optics.

[12]  H. Quenzel,et al.  Turbidity of the atmosphere determined from satellite: Calculation of optimum viewing geometry , 1979 .

[13]  E. M. Patterson,et al.  Complex Index of Refraction Between 300 and 700 nm for Saharan Aerosols , 1977 .

[14]  Robert Frouin,et al.  Determination from Space of Atmospheric Total Water Vapor Amounts by Differential Absorption near 940 nm: Theory and Airborne Verification , 1990 .

[15]  R. S. Fraser Satellite measurement of mass of Sahara dust in the atmosphere. , 1976, Applied optics.

[16]  E. Shettle,et al.  Optical and Radiative Properties of a Desert Aerosol Model , 1986 .

[17]  F. Bretherton,et al.  Cloud cover from high-resolution scanner data - Detecting and allowing for partially filled fields of view , 1982 .

[18]  Robert J. Curran,et al.  The detection of dust storms over land and water with satellite visible and infrared measurements , 1974 .

[19]  M. Desbois,et al.  The Potential of Infrared Satellite Data for the Retrieval of Saharan-Dust Optical Depth over Africa. , 1989 .

[20]  Yoram J. Kaufman,et al.  Satellite sensing of aerosol absorption , 1987 .

[21]  Didier Tanré,et al.  Radiative Properties of Desert Aerosols by Optical Ground-Based Measurements at Solar Wavelengths , 1988 .

[22]  Toby N. Carlson,et al.  Atmospheric Turbidity in Saharan Dust Outbreaks as Determined by Analyses of Satellite Brightness Data , 1979 .