| Literature DB >> 22936773 |
Christopher Pöhlker1, Kenia T Wiedemann, Bärbel Sinha, Manabu Shiraiwa, Sachin S Gunthe, Mackenzie Smith, Hang Su, Paulo Artaxo, Qi Chen, Yafang Cheng, Wolfgang Elbert, Mary K Gilles, Arthur L D Kilcoyne, Ryan C Moffet, Markus Weigand, Scot T Martin, Ulrich Pöschl, Meinrat O Andreae.
Abstract
The fine particles serving as cloud condensation nuclei in pristine Amazonian rainforest air consist mostly of secondary organic aerosol. Their origin is enigmatic, however, because new particle formation in the atmosphere is not observed. Here, we show that the growth of organic aerosol particles can be initiated by potassium-salt-rich particles emitted by biota in the rainforest. These particles act as seeds for the condensation of low- or semi-volatile organic compounds from the atmospheric gas phase or multiphase oxidation of isoprene and terpenes. Our findings suggest that the primary emission of biogenic salt particles directly influences the number concentration of cloud condensation nuclei and affects the microphysics of cloud formation and precipitation over the rainforest.Entities:
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Year: 2012 PMID: 22936773 DOI: 10.1126/science.1223264
Source DB: PubMed Journal: Science ISSN: 0036-8075 Impact factor: 47.728