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Dependence of solar radiative forcing of forest fire aerosol on ageing and state of mixture

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Fig. 1. Particle number size distributions within the upper sub- sub-layer (red data points) and lower sub-sub-layer (black data points) of the aerosol from biomass-burning over Lindenberg, Germany on 9 August 1998
Fig. 2. Comparison of spectral lidar backscatter coefficient for lower sub-layer during the night from 9 to 10 August 1998,  calcu-lated from in-situ measurements of the particle microphysical  prop-erties and measured by the IfT multi-wavelength lidar (qu
Table 2. Compilation of Parameters of Log-Normal Distributions Fitted to Accumulation Mode Particle Size Distributions Measured in Aerosols Originating from Forest or Vegetation Fires.
Fig. 3. Temporal development of accumulation mode median di- di-ameter for an aerosol from biomass-burning due to coagulation for different assumptions on initial concentration and dispersion during ageing.
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