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Impacts of convective storms on bioaerosol properties
Dissertation

Impacts of convective storms on bioaerosol properties

Teresa K. Feldman
University of Iowa
Doctor of Philosophy (PhD), University of Iowa
Spring 2026
DOI: 10.25820/etd.008413
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Teresa_Feldman_Thesis_20260501_Final16.32 MB
Embargoed Access, Embargo ends: 06/29/2028

Abstract

Biological particles suspended in the atmosphere, also known as bioaerosols, include pollen, bacteria, and fungal spores. Bioaerosols affect the climate and public health through properties including size, ice nucleating ability, and allergens and toxins. With a focus on fungal spores, bacteria, and pollen, this thesis advances understanding of how convective storm-generated cold pools and precipitation impact bioaerosol concentrations and size distributions. These bioaerosol properties and their temporal variation are essential to characterize, because they affect particle lifetime, their deposition in the respiratory tract, and their ability to affect cloud microphysics as ice nucleating particles.To characterize convective storm impacts on bioaerosols, samples and data were collected in a semi-arid grassland environment as a part of the BioAerosols and Convective Storms (BACS) field campaigns in May – June of 2022 (BACS-I) and 2023 (BACS-II) at the Central Plains Experimental Range in Northern Colorado. Convective storm impacts on bioaerosol sizes, concentrations, and types were characterized through a combination of highly time resolved online measurements and molecular-level offline analysis. Daily samples were collected for offline analysis of chemical tracers, ice nucleating particles, pollen, and fungal spores. Single particle fluorescence spectroscopy provided minute-averaged concentrations of fluorescent particles as a proxy for bioaerosols. Storm-generated cold pools and precipitation demonstrated significant impacts on bioaerosol properties at the CPER site. BACS-I had drought-like conditions and higher concentrations of endotoxin from gram-negative bacteria, while BACS-II had near record rainfall and higher concentrations of mannitol, a fungal spore tracer. For both campaigns, most precipitation events increased fungal spores, based on mannitol concentrations, microscope analysis of spores, and fluorescent particles. Storm-generated cold pools typically enhanced bioaerosol concentrations, with stronger cold pools, as indicated by perturbations of temperature, humidity, and wind speed, increasing bioaerosol concentrations more than weaker cold pools. Propagating speeds, a robust measure of cold pool strength, correlated significantly with peak fluorescent particle concentrations across both campaigns, further supporting the connection between cold pool strength and the magnitude of bioaerosol response. Increases in ice nucleating particles at warm temperatures (-15 C) coincided with convective storms and correlated with mannitol (2.5-10 µm), consistent with fungal spore contributions to ice nuclei. The effects of convective storms on bioaerosol size distributions were examined for cold pools with and without precipitation. The gust front of a dust storm increased total bioaerosols and particulate matter with no observed bioaerosol enrichment in coarse particles (2.5-10 µm), consistent with lofting of surface particles by strong winds. Cold pools without rainfall enriched coarse mode bioaerosols associated with fungal spores through microscopy and fluorescent particle signatures. Rainfall increased bioaerosol concentrations, adding a fine mode (1-2.5 µm) of bioaerosols compared to cold pools with no rain. In gust fronts, and cold pools with and without precipitation, fungal spores were the dominant bioaerosol type by number in coarse particles. The fine and coarse bioaerosols associated with storms are of sufficient size to enter the respiratory tract, with fine particles able to penetrate deeper and having higher deposition probabilities. This thesis advances our understanding of how convective cold pools and precipitation impact bioaerosols and biological ice nuclei. The outcomes of this research will aid in future work to constrain bioaerosol emissions and transport during convective storms by demonstrating fungal spore concentrations can be significantly enhanced in storm-generated cold pools and precipitation, each with distinct size distributions. Significant differences in fungal spore composition between campaigns also provides insight into the impacts of longer-term meteorological conditions on bioaerosol populations. More accurate representation of bioaerosol concentrations and sizes can help to inform strategies to mitigate harmful bioaerosol exposures for sensitive populations and to assess the impacts of storm-generated bioaerosols on cloud processes.
Atmospheric Sciences Precipitation Bioaerosols Cold pools Convective storms Fungal spores Wideband Integrated Bioaerosol Sensor

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