Articles | Volume 13, issue 5
Atmos. Chem. Phys., 13, 2391–2413, 2013

Special issue: European Integrated Project on Aerosol-Cloud-Climate and Air...

Atmos. Chem. Phys., 13, 2391–2413, 2013

Research article 01 Mar 2013

Research article | 01 Mar 2013

Long term measurements of aerosol optical properties at a primary forest site in Amazonia

L. V. Rizzo1, P. Artaxo2, T. Müller3, A. Wiedensohler3, M. Paixão3, G. G. Cirino4, A. Arana2, E. Swietlicki5, P. Roldin5, E. O. Fors5, K. T. Wiedemann6, L. S. M. Leal4, and M. Kulmala7 L. V. Rizzo et al.
  • 1Department of Earth and Exact Sciences, Institute of Environmental, Chemical and Pharmaceutics Sciences, Federal University of São Paulo, Sao Paulo, Brazil
  • 2Department of Applied Physics, Institute of Physics, University of São Paulo, Sao Paulo, Brazil
  • 3Leibniz Institute for Tropospheric Research, Leipzig, Germany
  • 4National Institute for Amazonian Research (INPA), Manaus, Brazil
  • 5Division of Nuclear Physics, Physics Institute, Lund University, Lund, Sweden
  • 6Division of Engineering and Applied Science/Department of Earth and Planetary Science, Harvard University, Cambridge, USA
  • 7Department of Physical Sciences, Division of Atmospheric Sciences, University of Helsinki, Helsinki, Finland

Abstract. A long term experiment was conducted in a primary forest area in Amazonia, with continuous in-situ measurements of aerosol optical properties between February 2008 and April 2011, comprising, to our knowledge, the longest database ever in the Amazon Basin. Two major classes of aerosol particles, with significantly different optical properties were identified: coarse mode predominant biogenic aerosols in the wet season (January–June), naturally released by the forest metabolism, and fine mode dominated biomass burning aerosols in the dry season (July–December), transported from regional fires. Dry particle median scattering coefficients at the wavelength of 550 nm increased from 6.3 Mm−1 to 22 Mm−1, whereas absorption at 637 nm increased from 0.5 Mm−1 to 2.8 Mm−1 from wet to dry season. Most of the scattering in the dry season was attributed to the predominance of fine mode (PM2) particles (40–80% of PM10 mass), while the enhanced absorption coefficients are attributed to the presence of light absorbing aerosols from biomass burning. As both scattering and absorption increased in the dry season, the single scattering albedo (SSA) did not show a significant seasonal variability, in average 0.86 ± 0.08 at 637 nm for dry aerosols. Measured particle optical properties were used to estimate the aerosol forcing efficiency at the top of the atmosphere. Results indicate that in this primary forest site the radiative balance was dominated by the cloud cover, particularly in the wet season. Due to the high cloud fractions, the aerosol forcing efficiency absolute values were below −3.5 W m−2 in 70% of the wet season days and in 46% of the dry season days. Besides the seasonal variation, the influence of out-of-Basin aerosol sources was observed occasionally. Periods of influence of the Manaus urban plume were detected, characterized by a consistent increase on particle scattering (factor 2.5) and absorption coefficients (factor 5). Episodes of biomass burning and mineral dust particles advected from Africa were observed between January and April, characterized by enhanced concentrations of crustal elements (Al, Si, Ti, Fe) and potassium in the fine mode. During these episodes, median particle absorption coefficients increased by a factor of 2, whereas median SSA values decreased by 7%, in comparison to wet season conditions.

Final-revised paper