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Investigating biomass burning aerosol morphology using a laser imaging nephelometer
Particle morphology is an important parameter affecting aerosol optical properties that are relevant to climate and air quality, yet it is poorly constrained due to sparse in situ measurements. Biomass burning is a large source of aerosol that generates particles with different morphologies. Quantif...
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Published in: | Atmospheric chemistry and physics 2018-02, Vol.18 (3), p.1879-1894 |
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Main Authors: | , , , , , , , , , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | Particle morphology is an important parameter affecting aerosol
optical properties that are relevant to climate and air quality, yet it is
poorly constrained due to sparse in situ measurements. Biomass burning is a
large source of aerosol that generates particles with different morphologies.
Quantifying the optical contributions of non-spherical aerosol populations is
critical for accurate radiative transfer models, and for correctly
interpreting remote sensing data. We deployed a laser imaging nephelometer at
the Missoula Fire Sciences Laboratory to sample biomass burning aerosol from
controlled fires during the FIREX intensive laboratory study. The laser
imaging nephelometer measures the unpolarized scattering phase function of an
aerosol ensemble using diode lasers at 375 and 405 nm. Scattered light from
the bulk aerosol in the instrument is imaged onto a charge-coupled device
(CCD) using a wide-angle
field-of-view lens, which allows for measurements at 4–175∘
scattering angle with ∼ 0.5∘ angular resolution. Along with a
suite of other instruments, the laser imaging nephelometer sampled fresh
smoke emissions both directly and after removal of volatile components with a
thermodenuder at 250 ∘C. The total integrated aerosol scattering
signal agreed with both a cavity ring-down photoacoustic spectrometer system
and a traditional integrating nephelometer within instrumental uncertainties.
We compare the measured scattering phase functions at 405 nm to theoretical
models for spherical (Mie) and fractal (Rayleigh–Debye–Gans) particle
morphologies based on the size distribution reported by an optical particle
counter. Results from representative fires demonstrate that particle
morphology can vary dramatically for different fuel types. In some cases, the
measured phase function cannot be described using Mie theory. This study
demonstrates the capabilities of the laser imaging nephelometer instrument to
provide realtime, in situ information about dominant particle morphology,
which is vital for understanding remote sensing data and accurately
describing the aerosol population in radiative transfer calculations. |
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ISSN: | 1680-7324 1680-7316 1680-7324 |
DOI: | 10.5194/acp-18-1879-2018 |