Abstract

Abstract. Aerosol fluxes were measured above a mixed forest by Eddy Covariance (EC) with a Fast Mobility Particle Sizer (FMPS) at the Borden Forest Research Station in Ontario, Canada between 13 July and 12 August 2009. Chemically speciated flux measurements were made at a height of 29 m at the same location between 19 July and 2 August, 2006 using a Quadrupole Aerosol Mass Spectrometer (Q-AMS). The Q-AMS measured an average sulphate deposition velocity of 0.3 mm s−1 and an average nitrate deposition velocity of 4.8 mm s−1. The FMPS, mounted at a height of 33 m (approximately 10 m above the canopy top) and housed in a temperature controlled enclosure, measured size-resolved particle concentrations from 3 to 410 nm diameter at a rate of 1 Hz. For the size range 18 < D < 452 nm, 60 % of fluxes were upward. The exchange velocity was between −0.5 and 2.0 mm s−1, with median values near 0.5 mm s−1 for all sizes between 22 and 310 nm. The size distribution of the apparent production rate of particles at 33 m peaked at a diameter of 75 nm. Results indicate a decoupling of the above and below canopy spaces, whereby particles are stored in the canopy space at night, and are then diluted with cleaner air above during the day.

Highlights

  • Atmospheric aerosol particles are generated by both anthropogenic and natural sources and through chemical and physical processes in the atmosphere

  • The fraction of upward fluxes seen in this study (60 %) is higher than any previously reported fractions over forests, which range near 20 % (Gronholm et al, 2007) to over 40 % (Pryor et al, 2008c)

  • The forest is a source of particles at this location with an average source rate of 3.1 × 106 particles m−2 s−1 for particles 18 < D < 452 nm

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Summary

Introduction

Atmospheric aerosol particles are generated by both anthropogenic and natural sources and through chemical and physical processes in the atmosphere. The sizes of airborne aerosols range from a few nanometers to tens of micrometers. The dynamics of atmospheric aerosols is highly complex, involving particle formation, growth, and surface exchange processes. Effects of aerosols include direct and indirect climate forcing (Forster et al, 2007) through the absorption and scattering of incoming solar radiation and the forma-. Aerosols are carriers of compounds containing nitrogen (N), sulphur (S), and other elements over large distances. The eventual deposition of sulphate (SO24−) and nitrate (NO−3 ) aerosols can lead to acidification of the environment and the deposition of nitrate can lead to eutrophication, especially in sensitive ecosystems (Spranger et al, 2004)

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