Please use this identifier to cite or link to this item: http://hdl.handle.net/123456789/2858
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dc.contributor.authorSinha, B.-
dc.date.accessioned2020-12-09T05:29:38Z-
dc.date.available2020-12-09T05:29:38Z-
dc.date.issued2013-
dc.identifier.citationAtmospheric Chemistry and Physics, 13(13), pp.6151-6164.en_US
dc.identifier.otherhttps://doi.org/10.5194/acp-13-6151-2013-
dc.identifier.urihttps://acp.copernicus.org/articles/13/6151/2013/-
dc.identifier.urihttp://hdl.handle.net/123456789/2858-
dc.descriptionOnly IISERM authors are available in the record.-
dc.description.abstractBioaerosols 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.en_US
dc.language.isoenen_US
dc.publisherEuropean Geosciences Unionen_US
dc.subjectClimate systemen_US
dc.subjectBioaerosolsen_US
dc.subjectPublic healthen_US
dc.titleHigh concentrations of biological aerosol particles and ice nuclei during and after rainen_US
dc.typeArticleen_US
Appears in Collections:Research Articles

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