Seasonal Variability of Aerosol Single Scattering Albedo at Biomass Burning Sites in Southern Africa and Amazonia
dc.contributor.author | Eck, Thomas | |
dc.contributor.author | Holben, Brent | |
dc.contributor.author | Mukelabai, M. | |
dc.contributor.author | Dubovik, Oleg | |
dc.contributor.author | Smirnov, Alexander | |
dc.contributor.author | Schafer, J. | |
dc.contributor.author | Slutsker, I. | |
dc.date.accessioned | 2024-04-29T17:02:50Z | |
dc.date.available | 2024-04-29T17:02:50Z | |
dc.date.issued | 2011-12-01 | |
dc.description.abstract | Monitoring of the optical properties of primarily biomass burning aerosols in Mongu, Zambia was initiated in 1995, when an AERONET sun/sky radiometer site was established at the Mongu airport. For the biomass burning season months (July-November), we present monthly means of aerosol single scattering albedo (SSA), aerosol size distributions, and refractive indices from almucantar sky scan retrievals utilizing the algorithm of Dubovik and King (2000). The monthly mean single scattering albedo at 440 nm in Mongu was found to increase significantly from July (0.845) to October (0.93). The slope of the spectral dependence of aerosol single scattering albedo with wavelength decreased as SSA increased from July to October. However, there was no significant change in particle size in either the dominant accumulation or secondary coarse modes during these months. Similarly, seasonal SSA retrievals for Etosha Pan, Namibia also show increasing values through the burning season in 2000. We also analyze the seasonality of SSA for sites in biomass burning regions of Amazonia. We show maps of satellite detected fire counts which indicate that the regions of primary biomass burning shift significantly from July to October. Possible reasons for the seasonal changes in observed SSA include differences in aging to due transport speed and distance from source regions, differences in biomass fuel types in different regions (fraction of woody biomass versus grasses), and differences in fuel moisture content (October is the beginning of the rainy season on both continents). | |
dc.description.sponsorship | The AERONET project was supported by Michael D. King, retired in 2008 from the NASA EOS project office, and subsequently by Hal B. Maring, Radiation Sciences Program, NASA Headquarters. We acknowledge Johan Le Roux of the Etosha Ecological Institute, Okuakuejo, Namibia, for the site management of the Etosha Pan AERONET site, and Bibi Bengis (South Africa National Parks) and Thomas Bigala for the site management of the Skukuza AERONET site. | |
dc.format.extent | 20 pages | |
dc.genre | journal articles | |
dc.genre | preprints | |
dc.identifier | doi:10.13016/m2llro-xxi3 | |
dc.identifier.uri | http://hdl.handle.net/11603/33556 | |
dc.language.iso | en_US | |
dc.relation.isAvailableAt | The University of Maryland, Baltimore County (UMBC) | |
dc.relation.ispartof | UMBC GESTAR II | |
dc.relation.ispartof | UMBC Faculty Collection | |
dc.rights | This 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.rights | Public Domain | |
dc.rights.uri | https://creativecommons.org/publicdomain/mark/1.0/ | |
dc.title | Seasonal Variability of Aerosol Single Scattering Albedo at Biomass Burning Sites in Southern Africa and Amazonia | |
dc.type | Text | |
dcterms.creator | https://orcid.org/0000-0001-9801-1610 |
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