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dc.contributor.authorPerring, A. E.
dc.contributor.authorSchwarz, J. P.
dc.contributor.authorBaumgardner, D.
dc.contributor.authorHernandez, M. T.
dc.contributor.authorSpracklen, D. V.
dc.contributor.authorGao, R. S.
dc.contributor.authorKok, G.
dc.contributor.authorMcMeeking, G. R.
dc.contributor.authorMcQuaid, J. B.
dc.contributor.authorFahey, D. W.
dc.contributor.authorHeald, Colette L.
dc.date.accessioned2016-03-08T01:10:32Z
dc.date.available2016-03-08T01:10:32Z
dc.date.issued2015-02
dc.date.submitted2014-08
dc.identifier.issn2169897X
dc.identifier.issn2169-8996
dc.identifier.urihttp://hdl.handle.net/1721.1/101627
dc.description.abstractAirborne observations of fluorescent aerosol were made aboard an airship during CloudLab, a series of flights that took place in September and October of 2013 and covered a wideband of longitude across the continental U.S. between Florida and California and between 28 and 37 N latitudes. Sampling occurred from near the surface to 1000 m above the ground. A Wideband Integrated Bioaerosol Sensor (WIBS-4) measured average concentrations of supermicron fluorescent particles aloft (1 µm to 10 µm), revealing number concentrations ranging from 2.1 ± 0.8 to 8.7 ± 2.2 × 10[superscript 4] particles m[superscript −3] and representing up to 24% of total supermicron particle number. We observed distinct variations in size distributions and fluorescent characteristics in different regions, and attribute these to geographically diverse bioaerosol. Fluorescent aerosol detected in the east is largely consistent with mold spores observed in a laboratory setting, while a shift to larger sizes associated with different fluorescent patterns is observed in the west. Fluorescent bioaerosol loadings in the desert west were as high as those near the Gulf of Mexico, suggesting that bioaerosol is a substantial component of supermicron aerosol both in humid and arid environments. The observations are compared to model fungal and bacterial loading predictions, and good agreement in both particle size and concentrations is observed in the east. In the west, the model underestimated observed concentrations by a factor between 2 and 4 and the prescribed particle sizes are smaller than the observed fluorescent aerosol. A classification scheme for use with WIBS data is also presented.en_US
dc.description.sponsorshipNational Science Foundation (U.S.) (AGS-1238109)en_US
dc.language.isoen_US
dc.publisherAmerican Geophysical Union (AGU)en_US
dc.relation.isversionofhttp://dx.doi.org/10.1002/2014JD022495en_US
dc.rightsArticle is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use.en_US
dc.sourceMIT web domainen_US
dc.titleAirborne observations of regional variation in fluorescent aerosol across the United Statesen_US
dc.typeArticleen_US
dc.identifier.citationPerring, A. E., J. P. Schwarz, D. Baumgardner, M. T. Hernandez, D. V. Spracklen, C. L. Heald, R. S. Gao, et al. “Airborne Observations of Regional Variation in Fluorescent Aerosol Across the United States.” J. Geophys. Res. Atmos. 120, no. 3 (February 3, 2015): 1153–1170. © 2014 American Geophysical Unionen_US
dc.contributor.departmentMassachusetts Institute of Technology. Department of Civil and Environmental Engineeringen_US
dc.contributor.mitauthorHeald, Colette L.en_US
dc.relation.journalJournal of Geophysical Research: Atmospheresen_US
dc.eprint.versionFinal published versionen_US
dc.type.urihttp://purl.org/eprint/type/JournalArticleen_US
eprint.statushttp://purl.org/eprint/status/PeerRevieweden_US
dspace.orderedauthorsPerring, A. E.; Schwarz, J. P.; Baumgardner, D.; Hernandez, M. T.; Spracklen, D. V.; Heald, C. L.; Gao, R. S.; Kok, G.; McMeeking, G. R.; McQuaid, J. B.; Fahey, D. W.en_US
dc.identifier.orcidhttps://orcid.org/0000-0003-2894-5738
mit.licensePUBLISHER_POLICYen_US
mit.metadata.statusComplete


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