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dc.contributor.authorGarimella, Sarvesh
dc.contributor.authorRothenberg, Daniel A.
dc.contributor.authorWolf, Martin J.
dc.contributor.authorDavid, Robert O.
dc.contributor.authorKanji, Zamin A.
dc.contributor.authorWang, Chien
dc.contributor.authorRösch, Michael
dc.contributor.authorCziczo, Daniel James
dc.date.accessioned2018-04-25T20:53:06Z
dc.date.available2018-04-25T20:53:06Z
dc.date.issued2017-09
dc.date.submitted2017-05
dc.identifier.issn1680-7324
dc.identifier.issn1680-7316
dc.identifier.urihttp://hdl.handle.net/1721.1/114963
dc.description.abstractThis study investigates the measurement of ice nucleating particle (INP) concentrations and sizing of crystals using continuous flow diffusion chambers (CFDCs). CFDCs have been deployed for decades to measure the formation of INPs under controlled humidity and temperature conditions in laboratory studies and by ambient aerosol populations. These measurements have, in turn, been used to construct parameterizations for use in models by relating the formation of ice crystals to state variables such as temperature and humidity as well as aerosol particle properties such as composition and number. We show here that assumptions of ideal instrument behavior are not supported by measurements made with a commercially available CFDC, the SPectrometer for Ice Nucleation (SPIN), and the instrument on which it is based, the Zurich Ice Nucleation Chamber (ZINC). Non-ideal instrument behavior, which is likely inherent to varying degrees in all CFDCs, is caused by exposure of particles to different humidities and/or temperatures than predicated from instrument theory of operation. This can result in a systematic, and variable, underestimation of reported INP concentrations. We find here variable correction factors from 1.5 to 9.5, consistent with previous literature values. We use a machine learning approach to show that non-ideality is most likely due to small-scale flow features where the aerosols are combined with sheath flows. Machine learning is also used to minimize the uncertainty in measured INP concentrations. We suggest that detailed measurement, on an instrument-by-instrument basis, be performed to characterize this uncertainty.en_US
dc.description.sponsorshipUnited States. National Aeronautics and Space Administration (Grant NNX13AO15G)en_US
dc.description.sponsorshipNational Science Foundation (U.S.) (Grant AGS-1461347)en_US
dc.description.sponsorshipNational Science Foundation (U.S.) (Grant AGS-1339264)en_US
dc.description.sponsorshipUnited States. Department of Energy (Award DE-SC0014487)en_US
dc.publisherCopernicus Publicationsen_US
dc.relation.isversionofhttp://dx.doi.org/10.5194/ACP-17-10855-2017en_US
dc.rightsCreative Commons Attribution 3.0 Unported licenseen_US
dc.rights.urihttp://creativecommons.org/licenses/by/3.0/en_US
dc.sourceCopernicus Publicationsen_US
dc.titleUncertainty in counting ice nucleating particles with continuous flow diffusion chambersen_US
dc.typeArticleen_US
dc.identifier.citationGarimella, Sarvesh et al. “Uncertainty in Counting Ice Nucleating Particles with Continuous Flow Diffusion Chambers.” Atmospheric Chemistry and Physics 17, 17 (September 2017): 10855–10864 © 2017 Author(s)en_US
dc.contributor.departmentMassachusetts Institute of Technology. Department of Civil and Environmental Engineeringen_US
dc.contributor.departmentMassachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciencesen_US
dc.contributor.mitauthorCziczo, Daniel James
dc.relation.journalAtmospheric Chemistry and Physicsen_US
dc.eprint.versionFinal published versionen_US
dc.type.urihttp://purl.org/eprint/type/JournalArticleen_US
eprint.statushttp://purl.org/eprint/status/PeerRevieweden_US
dc.date.updated2018-04-24T14:00:01Z
dspace.orderedauthorsGarimella, Sarvesh; Rothenberg, Daniel A.; Wolf, Martin J.; David, Robert O.; Kanji, Zamin A.; Wang, Chien; Rösch, Michael; Cziczo, Daniel J.en_US
dspace.embargo.termsNen_US
dc.identifier.orcidhttps://orcid.org/0000-0003-1851-8740
mit.licensePUBLISHER_CCen_US


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