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AGU: Geophysical Research Letters

 

Index Terms

  • Atmospheric Composition and Structure: Aerosols and particles
  • Atmospheric Composition and Structure: Cloud/radiation interaction
  • Atmospheric Processes: Clouds and aerosols
  • Atmospheric Processes: Radiative processes

Abstract

GEOPHYSICAL RESEARCH LETTERS, VOL. 32, L12819, 4 PP., 2005
doi:10.1029/2005GL022678

Laboratory measurements of smoke optical properties from the burning of Indonesian peat and other types of biomass

D. Chand

Biogeochemistry Department, Max Planck Institute for Chemistry, Mainz, Germany

O. Schmid

Biogeochemistry Department, Max Planck Institute for Chemistry, Mainz, Germany

P. Gwaze

Biogeochemistry Department, Max Planck Institute for Chemistry, Mainz, Germany

R. S. Parmar

Biogeochemistry Department, Max Planck Institute for Chemistry, Mainz, Germany

G. Helas

Biogeochemistry Department, Max Planck Institute for Chemistry, Mainz, Germany

K. Zeromskiene

Institute for Tropospheric Research, Leipzig, Germany

A. Wiedensohler

Institute for Tropospheric Research, Leipzig, Germany

A. Massling

Institute for Tropospheric Research, Leipzig, Germany

M. O. Andreae

Biogeochemistry Department, Max Planck Institute for Chemistry, Mainz, Germany

We present the first results on optical properties (λ ∼ 540 nm) of fresh aerosols from the combustion of Indonesian peat, German peat and other types of biomass, measured under controlled laboratory conditions. The mass scattering and mass absorption efficiencies for Indonesian and German peat aerosols are in the range of 6.0–8.1 and 0.04–0.06 m2 g−1, respectively. A very high single scattering albedo (0.99) is observed for the peat smoke aerosols, reflecting the smoldering burning conditions (emission ratio, ΔCO/ΔCO2 = 19–50%). The relative increase in light scattering (f(RH)) due to an increase in relative humidity (RH) from 15% to 90% is very low (i.e., f(90) = 1.05) for both Indonesian and German peat aerosols. This value is considerably smaller than for aged Indonesian peat smoke particles (f(80) = 1.65) [Gras et al., 1999]. This suggests that atmospheric aging processes may be an important factor for aerosol hygroscopicity.

Received 10 February 2005; accepted 13 May 2005; published 30 June 2005.

Citation: Chand, D., O. Schmid, P. Gwaze, R. S. Parmar, G. Helas, K. Zeromskiene, A. Wiedensohler, A. Massling, and M. O. Andreae (2005), Laboratory measurements of smoke optical properties from the burning of Indonesian peat and other types of biomass, Geophys. Res. Lett., 32, L12819, doi:10.1029/2005GL022678.

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