Influx of African biomass burning aerosol during the Amazonian dry season through layered transatlantic transport of black carbon-rich smoke

Black carbon (BC) aerosols influence the Earth's atmosphere and climate, but their microphysical properties, spatiotemporal distribution, and long-range transport are not well constrained. This study presents airborne observations of the transatlantic transport of BC-rich African biomass burnin...

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Veröffentlicht in:Atmospheric chemistry and physics 2020-04, Vol.20 (8), p.4757-4785
Hauptverfasser: Holanda, Bruna A, Pöhlker, Mira L, Walter, David, Saturno, Jorge, Sörgel, Matthias, Ditas, Jeannine, Ditas, Florian, Schulz, Christiane, Franco, Marco Aurélio, Wang, Qiaoqiao, Donth, Tobias, Artaxo, Paulo, Barbosa, Henrique M. J, Borrmann, Stephan, Braga, Ramon, Brito, Joel, Cheng, Yafang, Dollner, Maximilian, Kaiser, Johannes W, Klimach, Thomas, Knote, Christoph, Krüger, Ovid O, Fütterer, Daniel, Lavric, JoÅ¡t V, Ma, Nan, Machado, Luiz A. T, Ming, Jing, Morais, Fernando G, Paulsen, Hauke, Sauer, Daniel, Schlager, Hans, Schneider, Johannes, Su, Hang, Weinzierl, Bernadett, Walser, Adrian, Wendisch, Manfred, Ziereis, Helmut, Zöger, Martin, Pöschl, Ulrich, Andreae, Meinrat O, Pöhlker, Christopher
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Sprache:eng
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Zusammenfassung:Black carbon (BC) aerosols influence the Earth's atmosphere and climate, but their microphysical properties, spatiotemporal distribution, and long-range transport are not well constrained. This study presents airborne observations of the transatlantic transport of BC-rich African biomass burning (BB) smoke into the Amazon Basin using a Single Particle Soot Photometer (SP2) as well as several complementary techniques. We base our results on observations of aerosols and trace gases off the Brazilian coast onboard the HALO (High Altitude and LOng range) research aircraft during the ACRIDICON-CHUVA campaign in September 2014.
ISSN:1680-7324
1680-7316
1680-7324
DOI:10.5194/acp-20-4757-2020