4.7 Article

Distinguishing in-cloud and below-cloud short and distal N-sources from high-temporal resolution seasonal nitrate and ammonium deposition in Vienna, Austria

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ATMOSPHERIC ENVIRONMENT
卷 266, 期 -, 页码 -

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PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.atmosenv.2021.118740

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Rainout; Washout; Scavenging ratio; Nitrogen pollution; High-resolution sampling

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The study investigated the washout of reactive nitrogen in precipitation events in Vienna, Austria in 2019. Results showed systematic seasonal concentration variations of nitrogen species and the influence of rush-hour traffic on nitrogen scavenging processes. Monthly nitrate and ammonium deposition rates were reported, along with the proportions of N-species from different sources.
Reactive nitrogen (N-r: nitrate and ammonium) washout in Vienna (Austria) precipitation events were investigated in 2019. A total of 958 samples from 61 rain events representing >90% of annual precipitation were collected at 5-30 min intervals for nitrate (NO3-) and ammonium (NH4+) analyses and meteorological information. The data revealed systematic seasonal concentration variations for all N-r-species and a clear influence of rush-hour traffic on the kinetics of N-scavenging processes. The monthly nitrate and ammonium deposition was 0.69 +/- 0.21 kg ha(-1) month(-1) and 1.02 +/- 0.30 kg ha(-1) month(-1), respectively. Around 30% of nitrate and 20% of ammonium was dry deposition, and similar to 30% of each N-species was from distal sources associated with rainout processes. The half-life of below-cloud N-species were similar in the warmer seasons (1.7 +/- 0.2 h and 2.3 +/- 0.4 h for nitrate and ammonium). In winter, the ammonium half-life was significantly lower (1.4 h). N-r removal by wet-only in-cloud scavenging was slower than predicted by empirical models. HYSPLIT trajectory analysis revealed that N-r rainout from distal sources in spring had no prevailing direction, but higher N-r contributions were from N and W. In summer and winter, air masses from W, SW and SE were related to intense, medium, and low N-r contributions, respectively. The origin and path of these trajectories coincided with known NOx hotspots in Europe.

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