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Airborne observations of bioaerosol over the Southeast United States using a Wideband Integrated Bioaerosol Sensor

Authors :
Chelsea A. Corr
Bruce E. Anderson
Luke D. Ziemba
Edward L. Winstead
Gao Chen
Glenn S. Diskin
Armin Wisthaler
Suzanne Crumeyrolle
K. Lee Thornhill
Andreas J. Beyersdorf
R. Martin
Michael Shook
Tomas Mikoviny
Richard H. Moore
C. H. Hudgins
Source :
Journal of Geophysical Research: Atmospheres. 121:8506-8524
Publication Year :
2016
Publisher :
American Geophysical Union (AGU), 2016.

Abstract

Biological aerosols represent a diverse subset of particulate matter that is emitted directly to the atmosphere in the form of (but not limited to) bacteria, fungal spores, pollens, viruses, and plant debris. These particles can have local air quality implications, but potentially play a larger climate role by acting as efficient ice nucleating particles (INPs) and cloud condensation nuclei. We have deployed a Wideband Integrated Bioaerosol Sensor on the NASA DC-8 aircraft to (1) quantify boundary layer (BL) variability of fluorescent biological aerosol particle (FBAP) concentrations in the Southeast United States (SEUS), (2) link this variability explicitly to land cover heterogeneity in the region, and (3) examine the vertical profile of bioaerosols in the context of convective vertical redistribution. Flight-averaged FBAP concentrations ranged between 0.1 and 0.43 scm−3 (cm−3 at standard temperature and pressure) with relatively homogeneous concentrations throughout the region; croplands showed the highest concentrations in the BL (0.37 scm−3), and lowest concentrations were associated with evergreen forests (0.24 scm−3). Observed FBAP concentrations are in generally good agreement with model parameterized emission rates for bacteria, and discrepancies are likely the result of fungal spore contributions. Shallow convection in the region is shown to be a relatively efficient lofting mechanism as the vertical transport efficiency of FBAP is at least equal to black carbon aerosol, suggesting that ground-level FBAP survives transport into the free troposphere to be available for INP activation. Comparison of the fraction of coarse-mode particles that were biological (fFBAP) suggested that the SEUS (fFBAP = 8.5%) was a much stronger source of bioaerosols than long-range transport during a Saharan Air Layer (SAL) dust event (fFBAP = 0.17%) or summertime marine emissions in the Gulf of Mexico (fFBAP = 0.73%).

Details

ISSN :
2169897X
Volume :
121
Database :
OpenAIRE
Journal :
Journal of Geophysical Research: Atmospheres
Accession number :
edsair.doi...........e2b832062c9e942d4d91f87af87fe11a
Full Text :
https://doi.org/10.1002/2015jd024669