High concentrations of biological aerosol particles and ice nuclei during and after rain

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Abstract

Bioaerosols are relevant for public health and may play an important role in the climate system, but their atmospheric abundance, properties, and sources are not well understood. Here we show that the concentration of airborne biological particles in a North American forest ecosystem increases significantly during rain and that bioparticles are closely correlated with atmospheric ice nuclei (IN). The greatest increase of bioparticles and IN occurred in the size range of 2-6 μm, which is characteristic for bacterial aggregates and fungal spores. By DNA analysis we found high diversities of airborne bacteria and fungi, including groups containing human and plant pathogens (mildew, smut and rust fungi, molds, Enterobacteriaceae, Pseudomonadaceae). In addition to detecting known bacterial and fungal IN (Pseudomonas sp., Fusarium sporotrichioides), we discovered two species of IN-active fungi that were not previously known as biological ice nucleators (Isaria farinosa and Acremonium implicatum). Our findings suggest that atmospheric bioaerosols, IN, and rainfall are more tightly coupled than previously assumed. © 2013 Author(s).

Figures

  • Fig. 1. Aerial photos of site layout. (A) Approximate lay-out of sampler and instruments: (1) Inlet #4 [CFDC], (2) Inlets 1–3 [#1: UV-APS, #2: MOUDI, #3: Total aerosol impactor + stacked filter unit], (3) Andersen biosamplers, (4) High-volume samplers, (5) Leaf wetness sensor (LWS), (6) Disdrometer, (7) WIBS profiling unit on Chemistry Tower. Instruments and samplers associated with inlets 1–4 are located inside trailer (white box). Additional details regarding other instrumentation and lay-out at: http://web3.acd. ucar.edu/beachon/site-info.shtml. (B) Aerial photo showing region immediately surrounding Manitou Experimental Forest sampling site, including county road 67 crossing north through the photo. Black box shows approximate area of photo (A). Photos courtesy: J. Patton.
  • Fig. 2. Time series of measurement data showing repeated bursts of airborne biological particles with rain events. (A) Measured rainfall (dark blue crosses) and corresponding leaf wetness (light blue trace). (B) Concentrations (L−1) of supermicron fluorescent bioparticles (NF) and (C) total (NT) supermicron particles. (D) Fraction of fluorescent biological to total (NF/NT). (E) Size-resolved fluorescent bioparticle concentrations measured with the UV-APS instrument (color bar: dNF/dlogDA, L −1). Data are plotted against local time (Mountain Daylight Time, MDT). Rain data shown for non-zero values.
  • Fig. 3. Contrasting aerosol properties during dry periods and rain events. (A, B) Fluorescence microscope images of aerosol impactor samples. (C, D) Size distributions of ice nuclei observed at −15 ◦C in microscopic IN activation experiments (bars, left axis) and of fluorescent bioparticles detected by UV-APS (traces, right axis). (E, F) Number concentrations of ice nuclei observed at −25 ◦C in CFDC measurements plotted against fluorescent bioparticles detected by UV-APS (particle diameter < 2.4 µm). The displayed linear fits yield R2 correlation coefficients of (E) 0.003 and (F) 0.88.
  • Table 1. Number fraction of biological particles and mineral dust particles in aerosol samples collected during dry periods and rain events. The sample numbers S10, S12, S20, S23 refer to Nuclepore® filters analyzed by SEM (details specified in Sect. S1.4.1.3). The UV-APS data were averaged over periods matching the filter sample collection times. Fluorescent biological aerosol particles (FBAP), primary biological aerosol particles (PBAP).
  • Table 2. Number fraction of bioparticles on MOUDI stages 4 (3.2– 5.6 µm) and 5 (1.8–3.2 µm) of aerosol samples collected during a dry period (M28) and a rain event (M10). See SOM Sect. S1.4.1.1 for sampling dates. Estimates based on fluorescence microscopy.
  • Fig. 4. Size distributions of ice nuclei observed in microscopic IN activation experiments (A) at −15 ◦C and (B) at −20 ◦C for aerosol impactor samples collected during dry periods and rain events. (C) Size distribution of bioparticles measured by UV-APS during the same periods. See SOM Sect. S1.4.1.1 for sampling dates.
  • Fig. 5. IN activation curves from microscopic IN activation experiments with size-resolved aerosol samples (MOUDI stages). Upper panels (A, B) for samples collected during rain events, and lower panels (C, D) for samples collected during dry periods. Red traces show Stage 4 (3.2–5.6 µm), blue traces show Stage 5 (1.8–3.2 µm), brown traces show Stages 6–8, and gray traces show Stages 1–3. See SOM Sect. S1.4.1.1 for sampling dates.
  • Fig. 6. An estimate of the fraction of particles collected during rain events (M10, M26) that can serve as IN at −15 ◦C. IN concentrations were calculated from microscopic IN activation experiments and particle concentrations were calculated from UV-APS measurements. See SOM Sect. S1.4.1.1 for sampling dates. Note that the fraction of particles with IN activity is greater than 1 in 1000 for all particles > 2 µm and exceeds 1 in 100 for particles > 10 µm. Exponential curve shown to guide the eye.

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CITATION STYLE

APA

Huffman, J. A., Prenni, A. J., Demott, P. J., Pöhlker, C., Mason, R. H., Robinson, N. H., … Pöschl, U. (2013). High concentrations of biological aerosol particles and ice nuclei during and after rain. Atmospheric Chemistry and Physics, 13(13), 6151–6164. https://doi.org/10.5194/acp-13-6151-2013

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