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Unexpected seasonality in quantity and composition of Amazon rainforest air reactivity

A. C. Nölscher (), A. M. Yañez-Serrano, S. Wolff, A. Carioca de Araujo, J. V. Lavrič, J. Kesselmeier and J. Williams
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A. C. Nölscher: Max Planck Institute for Chemistry
A. M. Yañez-Serrano: Max Planck Institute for Chemistry
S. Wolff: Max Planck Institute for Chemistry
A. Carioca de Araujo: Embrapa Amazônia Oriental, Empresa Brasileira de Pesquisa Agropecuaria
J. V. Lavrič: Max Planck Institute for Biogeochemistry
J. Kesselmeier: Max Planck Institute for Chemistry
J. Williams: Max Planck Institute for Chemistry

Nature Communications, 2016, vol. 7, issue 1, 1-12

Abstract: Abstract The hydroxyl radical (OH) removes most atmospheric pollutants from air. The loss frequency of OH radicals due to the combined effect of all gas-phase OH reactive species is a measureable quantity termed total OH reactivity. Here we present total OH reactivity observations in pristine Amazon rainforest air, as a function of season, time-of-day and height (0–80 m). Total OH reactivity is low during wet (10 s−1) and high during dry season (62 s−1). Comparison to individually measured trace gases reveals strong variation in unaccounted for OH reactivity, from 5 to 15% missing in wet-season afternoons to mostly unknown (average 79%) during dry season. During dry-season afternoons isoprene, considered the dominant reagent with OH in rainforests, only accounts for ∼20% of the total OH reactivity. Vertical profiles of OH reactivity are shaped by biogenic emissions, photochemistry and turbulent mixing. The rainforest floor was identified as a significant but poorly characterized source of OH reactivity.

Date: 2016
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DOI: 10.1038/ncomms10383

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