Using Multi-Platform Satellite Observations to Study the Atmospheric Evolution of Brown Carbon in Siberian Biomass Burning Plumes

A bulk of evidence from in situ observations and lab experiments suggests that brown carbon (light-absorbing organic compounds in particles) can provide a significant yet highly variable contribution to the overall light absorption by aerosol particles from biomass burning (BB). Partly stemming from...

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Vydáno v:Remote sensing (Basel, Switzerland) Ročník 14; číslo 11; s. 2625
Hlavní autoři: Konovalov, Igor B., Golovushkin, Nikolai A., Beekmann, Matthias, Turquety, Solène
Médium: Journal Article
Jazyk:angličtina
Vydáno: Basel MDPI AG 31.05.2022
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ISSN:2072-4292, 2072-4292
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Abstract A bulk of evidence from in situ observations and lab experiments suggests that brown carbon (light-absorbing organic compounds in particles) can provide a significant yet highly variable contribution to the overall light absorption by aerosol particles from biomass burning (BB). Partly stemming from the complexity of the atmospheric evolution of organic aerosol (OA), the variability in brown carbon (BrC) absorption makes it difficult to partition the radiative effects of BrC and black carbon (BC) in atmospheric and climate models; as such, there are calls for satellite-based methods that could provide a statistical characterization of BrC absorption and its evolution in different regions of the world, especially in remote BB regions, such as Siberia. This study examined the feasibility of the statistical characterization of the evolution of BrC absorption and related parameters of BB aerosol in smoke plumes from intense wildfires in Siberia through the analysis of a combination of data from three satellite instruments: OMI (Ozone Monitoring Instrument), MISR (Multi-Angle Imaging SpectroRadiometer), and MODIS (Moderate Resolution Imaging Spectroradiometer). Using a Monte Carlo method, which related the satellite retrievals of the absorption and extinction aerosol optical depths to Mie theory calculations of the optical properties of BB aerosol, we found that the BrC absorption, as well as the imaginary refractive index for the OA, decreased significantly in Siberian BB smoke plumes during about 30 h of the daylight evolution, nevertheless remaining considerable until at least 70 h of the daylight evolution. Overall, the study indicated that the analysis of multi-platform satellite observations of BB plumes can provide useful insights into the atmospheric evolution of BrC absorption and the partitioning of BrC and BC contributions to the total light absorption by BB aerosol.
AbstractList A bulk of evidence from in situ observations and lab experiments suggests that brown carbon (light-absorbing organic compounds in particles) can provide a significant yet highly variable contribution to the overall light absorption by aerosol particles from biomass burning (BB). Partly stemming from the complexity of the atmospheric evolution of organic aerosol (OA), the variability in brown carbon (BrC) absorption makes it difficult to partition the radiative effects of BrC and black carbon (BC) in atmospheric and climate models; as such, there are calls for satellite-based methods that could provide a statistical characterization of BrC absorption and its evolution in different regions of the world, especially in remote BB regions, such as Siberia. This study examined the feasibility of the statistical characterization of the evolution of BrC absorption and related parameters of BB aerosol in smoke plumes from intense wildfires in Siberia through the analysis of a combination of data from three satellite instruments: OMI (Ozone Monitoring Instrument), MISR (Multi-Angle Imaging SpectroRadiometer), and MODIS (Moderate Resolution Imaging Spectroradiometer). Using a Monte Carlo method, which related the satellite retrievals of the absorption and extinction aerosol optical depths to Mie theory calculations of the optical properties of BB aerosol, we found that the BrC absorption, as well as the imaginary refractive index for the OA, decreased significantly in Siberian BB smoke plumes during about 30 h of the daylight evolution, nevertheless remaining considerable until at least 70 h of the daylight evolution. Overall, the study indicated that the analysis of multi-platform satellite observations of BB plumes can provide useful insights into the atmospheric evolution of BrC absorption and the partitioning of BrC and BC contributions to the total light absorption by BB aerosol.
Author Golovushkin, Nikolai A.
Konovalov, Igor B.
Beekmann, Matthias
Turquety, Solène
Author_xml – sequence: 1
  givenname: Igor B.
  orcidid: 0000-0002-0716-4273
  surname: Konovalov
  fullname: Konovalov, Igor B.
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  givenname: Nikolai A.
  surname: Golovushkin
  fullname: Golovushkin, Nikolai A.
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  givenname: Matthias
  surname: Beekmann
  fullname: Beekmann, Matthias
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  givenname: Solène
  surname: Turquety
  fullname: Turquety, Solène
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Issue 11
Keywords satellite observations of aerosol
Siberian wildfires
organic aerosol
aerosol absorption
aerosol atmospheric aging
biomass burning aerosol
MODIS
MISR
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Snippet A bulk of evidence from in situ observations and lab experiments suggests that brown carbon (light-absorbing organic compounds in particles) can provide a...
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SubjectTerms Absorption
aerosol absorption
Aerosols
Aircraft
Atmospheric aerosols
Atmospheric evolution
Atmospheric models
Biomass
Biomass burning
biomass burning aerosol
Black carbon
brown carbon
Burning
Carbon
Climate models
Daylight
Electromagnetic absorption
Environmental Sciences
Evolution
Feasibility studies
Forest & brush fires
Knowledge
Light
Mie scattering
Monitoring instruments
Monte Carlo simulation
Optical properties
organic aerosol
Organic compounds
Physics
Plumes
Refractivity
Regions
Remote sensing
Satellite instruments
Satellite observation
satellite observations of aerosol
Satellites
Siberian wildfires
Smoke
Spectroradiometers
Statistics
Wildfires
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Title Using Multi-Platform Satellite Observations to Study the Atmospheric Evolution of Brown Carbon in Siberian Biomass Burning Plumes
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