Search Results

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    Atmospheric new particle formation at Utö, Baltic Sea 2003-2005
    (Milton Park : Taylor & Francis, 2017) Hyvärinen, A.-P.; Komppula, M.; Engler, C.; Kivekäs, N.; Kerminen, V.-M.; Dal Maso, M.; Viisanen, Y.; Lihavainen, H.
    Nearly 3 yr (March 2003–December 2005) of continuous particle number size distribution measurements have been conducted at the island of Ut¨o in the Baltic Sea. The measured particle size range was from 7 to 530 nm. During the measurement period, a total of 103 regional new-particle formation events were observed. The characteristics of the nucleation events at Ut¨o were similar to those reported in the literature in other Nordic sites, though measured condensation sinks were rather high (geometric mean of 3.8 × 10−3 s−1) during event days. Clear evidence was found that new particles nucleate regionally near Ut¨o, rather than are transported from greater distances. However, the Baltic Sea seems to have an inhibiting effect on new-particle formation. The boreal forest areas in the continental Finland were found to have an enhancing effect on the nucleation probability in Ut¨o, suggesting that at least some of the precursor gases for nucleation and/or condensational growth of particles originate from these forests. In addition to regional new-particle formation events, a total of 94 local events were observed in Ut¨o. These are short-lived events with a small footprint area, and can at least partly be tracked down to the emissions of ship traffic operating at Ut¨o.
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    How to find bananas in the atmospheric aerosol': New approach for analyzing atmospheric nucleation and growth events
    (Milton Park : Taylor & Francis, 2017) Heintzenberg, Jost; Wehner, Birgit; Birmili, Wolfram
    We have devised a new search algorithm for secondary particle formation events, or ‘nucleation events’ in data sets of atmospheric particle size distributions. The search algorithm is simple and based on the investigation of 18 integral parameters of the particle size distribution, three of which were found to be most relevant for identifying nucleation events. The algorithm is tested using long-term size distribution data sets of high-size resolution observed at Melpitz, Hohenpeissenberg, and Leipzig, Germany, and Beijing, China, thereby covering a wide range of clean and polluted conditions. By specifying the particular training sets, the method can be used by other researchers with different data sets or different research goals. The same search approach could be applied to identify and analyze other systematic changes in size distribution such as during frontal passages or sand storms. As an example application of the new algorithm, the 50 strongest nucleation events (‘bananas’) at each of the four sites are analyzed statistically in terms of average changes of integral parameters of the particle size distribution.
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    The atmospheric aerosol over Siberia, as seen from the 300 m ZOTTO tower
    (Milton Park : Taylor & Francis, 2017) Heintzenberg, Jost; Birmili, Wolfram; Theiss, Detlef; Kisilyakhov, Yegor
    This report describes a unique setup for aerosol measurements at the new long-term Tall Tower monitoring facility near Zotino, Siberia (ZOTTO). Through two inlets at 50 and 300 m aerosol particle number size distributions are measured since September 2006 in the size range 15–835 nanometer dry diameter. Until the end of May 2007 total number (N300) concentrations at 300 m height ranged between 400 cm-3 (5%) and 4000 cm-3 (95%) with a median of 1200 cm-3, which is rather high for a nearly uninhabited boreal forest region during the low productivity period of the year. Fitting 1-h average distributions with a maximum of four lognormal functions yielded frequent ultrafine modes below 20 nm at 50 m height than at 300 m, whereas the latter height more frequently showed an aged nucleation mode near 30 nm. The positions of Aitken (≈80 nm) and accumulation modes (≈210 nm) were very similar at both inlet heights, the very sharp latter one being the most frequent of all modes. The encouraging first results let us expect exciting newfindings during the summer period with frequent forest fires and secondary particle sources from vegetation emissions.