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Abstract
Atmospheric black carbon (BC) has a strong positive, but still controversial, effect on global warming. In particular, BC absorption enhancement (Eabs) due to internal mixing with other chemical species—so-called lensing effect—is poorly assessed. This bottleneck partly relies on the lack of long-term in situ measurements of both the optical and chemical properties of BC-containing particles. Here, we present experimental and computational results showing a significant Eabs increase with the aerosol photochemical aging. This was associated with the production of highly oxidized secondary organic aerosols (SOA), especially at summertime. The 3-year-long continuous aerosol chemical and optical measurements used for the present study was obtained in the Paris region, France, which might be representative of near-future air quality within developing countries. These findings suggest that SOA could represent one of the most critical chemical species to be considered within climate models.
Atmospheric chemistry: organic aerosols amplify atmospheric warming from black carbon
Tiny remnants of combustion, known as black carbon, absorb solar radiation and warm the atmosphere—an effect that can be doubled by “lensing” from secondary organic aerosols. A multi-institution team led by Olivier Favez at the Institut National de l’Environnement Industriel et des Risques conducted a three-year observational and modeling study near Paris. The researchers tested a range of atmospheric constituents and found that secondary organic aerosols—adhered to black carbon particles—are the most important determinant of the enhanced warming. The aerosols are produced by photochemical reactions with a wide variety of natural and human-produced volatile organic compounds, and act to focus solar radiation to the core of the black carbon particle, especially during the particle aging process during summer. The findings—although specific to Paris—provide insights into the specific compounds leading to enhanced warming, and reveal the most effective targets for remediating their effect.
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1 Institut National de l’Environnement Industriel et des Risques, Verneuil-en-Halatte, France (GRID:grid.8453.a) (ISNI:0000 0001 2177 3043); Laboratoire des Sciences du Climat et de l’Environnement, CNRS-CEA-UVSQ, Gif-sur-Yvette, France (GRID:grid.457340.1) (ISNI:0000 0001 0584 9722)
2 Institut National de l’Environnement Industriel et des Risques, Verneuil-en-Halatte, France (GRID:grid.8453.a) (ISNI:0000 0001 2177 3043)
3 Paul Scherrer Institute, Laboratory of Atmospheric Chemistry, Villigen PSI, Switzerland (GRID:grid.5991.4) (ISNI:0000 0001 1090 7501)
4 University of Manchester, Centre for Atmospheric Sciences, School of Earth and Environmental Sciences, Manchester, UK (GRID:grid.5379.8) (ISNI:0000000121662407)
5 J. Stefan Institute, Condensed Matter Physics Department, Ljubljana, Slovenia (GRID:grid.11375.31) (ISNI:0000 0001 0706 0012)
6 The Cyprus Institute, Environment Energy and Water Research Center, Nicosia, Cyprus (GRID:grid.426429.f) (ISNI:0000 0004 0580 3152)
7 Laboratoire des Sciences du Climat et de l’Environnement, CNRS-CEA-UVSQ, Gif-sur-Yvette, France (GRID:grid.457340.1) (ISNI:0000 0001 0584 9722)