安静的
大气(单位)
事件(粒子物理)
粒子(生态学)
环境科学
白天
航程(航空)
大气科学
粒子数
气象学
物理
天体物理学
地质学
材料科学
天文
核物理学
等离子体
海洋学
复合材料
作者
Markku Kulmala,Heikki Junninen,Lubna Dada,Imre Salma,Tamás Weidinger,Wanda Thén,Máté Vörösmarty,Kaupo Komsaare,Dominik Stolzenburg,Runlong Cai,Chao Yan,Xinyang Li,Chenjuan Deng,Jingkun Jiang,Tuukka Petäjä,Tuomo Nieminen,Veli‐Matti Kerminen
标识
DOI:10.3389/fenvs.2022.912385
摘要
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.
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