Geophysical Research Letters · 1999 · 106 citations · 14 references
Natural SciencesEarth SciencesAtmospheric ChemistryAtmospheric ScienceCombustionAerosol PhysicsAtmospheric OpticsBiomass Burning EmissionsFire WeatherParticulate MatterSmog FormationAerosol Hygroscopic GrowthAerosol Optical PropertiesAerosol TransportFiresFlaming CombustionLower Atmosphere ChemistryOptical PropertiesSmoke Composition
Aerosol light‐scattering coefficient at 530 nm and its hygroscopic growth were determined in biomass‐burning smoke in the lower atmosphere over Kalimantan and northern Australia during the 1997 dry‐season fires. Both in and away from plumes, light‐scattering was considerably greater in the Indonesian region and hygroscopic growth in scattering was also consistently greater. The relative increase in scattering, from 20% to 80% relative humidity, was typically 1.37 in northern Australian and 1.65 in Kalimantan. Limited aerosol light absorption data indicate relatively small absorption in the Indonesian smoke. In part these differences can be explained by different combustion phases, mixed flaming and smoldering in the Australian savanna fires compared with predominantly smoldering in Indonesia, although these and other concurrent measurements suggest that underground peat combustion may have made a significant contribution to the Indonesian smoke.
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Biomass burning and global change
Joel S. Levine, Wesley R. Cofer, Donald R. Cahoon et al. · AIP conference proceedings · 1992 · 646 citations
Visibility forecast in the phase of pre-condensation
Fritz Kasten · Tellus · 1969 · 167 citations