Wavelength dependence of the optical depth of biomass burning, urban, and desert dust aerosols

dc.contributor.authorEck, Thomas
dc.contributor.authorHolben, B. N.
dc.contributor.authorReid, J. S.
dc.contributor.authorDubovik, O.
dc.contributor.authorSmirnov, A.
dc.contributor.authorO'Neill, N. T.
dc.contributor.authorSlutsker, I.
dc.contributor.authorKinne, S.
dc.date.accessioned2024-04-29T17:01:45Z
dc.date.available2024-04-29T17:01:45Z
dc.date.issued1999-12-01
dc.description.abstractThe 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 λ 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.
dc.description.urihttps://onlinelibrary.wiley.com/doi/abs/10.1029/1999JD900923
dc.format.extent17 pages
dc.genrejournal articles
dc.identifierdoi:10.13016/m2c1ni-9lr4
dc.identifier.citationEck, T.F., B. N. Holben, J. S. Reid, O. Dubovik, A. Smirnov, N. T. O’Neill, I. Slutsker, and S. Kinne. “Wavelength Dependence of the Optical Depth of Biomass Burning, Urban, and Desert Dust Aerosols.” Journal of Geophysical Research: Atmospheres 104, no. D24 (1999): 31333–49. https://doi.org/10.1029/1999JD900923.
dc.identifier.urihttps://doi.org/10.1029/1999JD900923
dc.identifier.urihttp://hdl.handle.net/11603/33462
dc.language.isoen_US
dc.publisherAGU
dc.relation.isAvailableAtThe University of Maryland, Baltimore County (UMBC)
dc.relation.ispartofUMBC GESTAR II
dc.rightsThis work was written as part of one of the author's official duties as an Employee of the United States Government and is therefore a work of the United States Government. In accordance with 17 U.S.C. 105, no copyright protection is available for such works under U.S. Law.
dc.rightsPublic Domain
dc.rights.urihttps://creativecommons.org/publicdomain/mark/1.0/
dc.titleWavelength dependence of the optical depth of biomass burning, urban, and desert dust aerosols
dc.typeText
dcterms.creatorhttps://orcid.org/0000-0001-9801-1610

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