Atmospheric new particle formation at the research station Melpitz, Germany: connection with gaseous precursors and meteorological parameters
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CitationGröß, J. Hamed, A. Sonntag, A. Spindler, G. Manninen, HE. Nieminen, T. Kulmala, M. Hõrrak, U. Plass-Dülmer, C. Wiedensohler, A. Birmili, W. (2018). Atmospheric new particle formation at the research station Melpitz, Germany: connection with gaseous precursors and meteorological parameters. ATMOSPHERIC CHEMISTRY AND PHYSICS, 18 (3) , 1835-1861. 10.5194/acp-18-1835-2018.
This paper revisits the atmospheric new particle formation (NPF) process in the polluted Central European troposphere, focusing on the connection with gas-phase precursors and meteorological parameters. Observations were made at the research station Melpitz (former East Germany) between 2008 and 2011 involving a neutral cluster and air ion spectrometer (NAIS). Particle formation events were classified by a new automated method based on the convolution integral of particle number concentration in the diameter interval 2–20 nm. To study the relevance of gaseous sulfuric acid as a precursor for nucleation, a proxy was derived on the basis of direct measurements during a 1-month campaign in May 2008. As a major result, the number concentration of freshly produced particles correlated significantly with the concentration of sulfur dioxide as the main precursor of sulfuric acid. The condensation sink, a factor potentially inhibiting NPF events, played a subordinate role only. The same held for experimentally determined ammonia concentrations. The analysis of meteorological parameters confirmed the absolute need for solar radiation to induce NPF events and demonstrated the presence of significant turbulence during those events. Due to its tight correlation with solar radiation, however, an independent effect of turbulence for NPF could not be established. Based on the diurnal evolution of aerosol, gas-phase, and meteorological parameters near the ground, we further conclude that the particle formation process is likely to start in elevated parts of the boundary layer rather than near ground level.