Author:
Kulmala Markku,Junninen Heikki,Dada Lubna,Salma Imre,Weidinger Tamás,Thén Wanda,Vörösmarty Máté,Komsaare Kaupo,Stolzenburg Dominik,Cai Runlong,Yan Chao,Li Xinyang,Deng Chenjuan,Jiang Jingkun,Petäjä Tuukka,Nieminen Tuomo,Kerminen Veli-Matti
Abstract
Atmospheric new particle formation (NPF) has been observed to take place in practice all around the world. In continental locations, typically about 10–40% of the days are so-called NPF event days characterized by a clear particle formation and growth that continue for several hours, occurring mostly during daytime. The other days are either non-event days, or days for which it is difficult to decide whether NPF had occurred or not. Using measurement data from several locations (Hyytiälä, Järvselja, and near-city background and city center of Budapest), we were able to show that NPF tends to occur also on the days traditionally characterized as non-event days. One explanation is the instrument sensitivity towards low number concentrations in the sub-10 nm range, which usually limits our capability to detect such NPF events. We found that during such days, particle formation rates at 6 nm were about 2–20% of those observed during the traditional NPF event days. Growth rates of the newly formed particles were very similar between the traditional NPF event and non-event days. This previously overlooked phenomenon, termed as quiet NPF, contributes significantly to the production of secondary particles in the atmosphere.
Funder
Academy of Finland
European Research Council
Subject
General Environmental Science
Cited by
13 articles.
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