Wavelength dependence of the optical depth of biomass burning, urban, and desert dust aerosols
- 27 December 1999
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research: Atmospheres
- Vol. 104 (D24) , 31333-31349
- https://doi.org/10.1029/1999jd900923
Abstract
The Angstrom wavelength exponent α, which is the slope of the logarithm of aerosol optical depth (τa) versus the logarithm of wavelength (λ), is commonly used to characterize the wavelength dependence of τa and to provide some basic information on the aerosol size distribution. This parameter is frequently computed from the spectral measurements of both ground‐based sunphotometers and from satellite and aircraft remote sensing retrievals. However, spectral variation of α is typically not considered in the analysis and comparison of values from different techniques. We analyze the spectral measurements of τa from 340 to 1020 nm obtained from ground‐based Aerosol Robotic Network radiometers located in various locations where either biomass burning, urban, or desert dust aerosols are prevalent. Aerosol size distribution retrievals obtained from combined solar extinction and sky radiance measurements are also utilized in the analysis. These data show that there is significant curvature in the ln τa versus ln λ relationship for aerosol size distributions dominated by accumulation mode aerosols (biomass burning and urban). Mie theory calculations of α for biomass burning smoke (for a case of aged smoke at high optical depth) agree well with observations, confirming that large spectral variations in α are due to the dominance of accumulation mode aerosols. A second order polynomial fit to the ln τa versus ln λ data provides excellent agreement with differences in τa of the order of the uncertainty in the measurements (∼0.01‐0.02). The significant curvature in ln τa versus ln λ for high optical depth accumulation mode dominated aerosols results in α values differing by a factor of 3–5 from 340 to 870 nm. We characterize the curvature in ln τa versus ln λ by the second derivative α′ and suggest that this parameter be utilized in conjunction with α to characterize the spectral dependence of τa. The second derivative of ln τa versus ln λ gives an indication of the relative influence of accumulation mode versus coarse mode particles on optical properties.This publication has 37 references indexed in Scilit:
- Wavelength dependence of the optical depth of biomass burning, urban, and desert dust aerosolsJournal of Geophysical Research: Atmospheres, 1999
- Use of the Ångstrom exponent to estimate the variability of optical and physical properties of aging smoke particles in BrazilJournal of Geophysical Research: Atmospheres, 1999
- Humidification factors of aerosols from biomass burning in BrazilJournal of Geophysical Research: Atmospheres, 1998
- Sphericity and morphology of smoke particles from biomass burning in BrazilJournal of Geophysical Research: Atmospheres, 1998
- Biomass burning aerosol size distribution and modeled optical propertiesJournal of Geophysical Research: Atmospheres, 1998
- Physical and optical properties of young smoke from individual biomass fires in BrazilJournal of Geophysical Research: Atmospheres, 1998
- Physical, chemical, and optical properties of regional hazes dominated by smoke in BrazilJournal of Geophysical Research: Atmospheres, 1998
- Measurements of irradiance attenuation and estimation of aerosol single scattering albedo for biomass burning aerosols in AmazoniaJournal of Geophysical Research: Atmospheres, 1998
- An overview of GOES‐8 diurnal fire and smoke results for SCAR‐B and 1995 fire season in South AmericaJournal of Geophysical Research: Atmospheres, 1998
- A use of two‐channel radiances for an aerosol characterization from spaceGeophysical Research Letters, 1998