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dc.contributor.authorSchiferl, Luke Daniel
dc.contributor.authorHeald, Colette L.
dc.contributor.authorNowak, John B.
dc.contributor.authorHolloway, John S.
dc.contributor.authorNeuman, J. Andrew
dc.contributor.authorBahreini, Roya
dc.contributor.authorPollack, Ilana B.
dc.contributor.authorRyerson, Thomas B.
dc.contributor.authorWiedinmyer, Christine
dc.contributor.authorMurphy, Jennifer G.
dc.date.accessioned2014-09-16T20:40:41Z
dc.date.available2014-09-16T20:40:41Z
dc.date.issued2014-02
dc.date.submitted2013-08
dc.identifier.issn2169897X
dc.identifier.urihttp://hdl.handle.net/1721.1/89665
dc.description.abstractAirborne observations from the California Research at the Nexus of Air Quality and Climate Change (CalNex) campaign in May and June 2010 are used to investigate the role of ammonia (NH3) in fine particulate matter (PM[subscript 2.5]) formation and surface air quality in California and test the key processes relevant to inorganic aerosol formation in the GEOS-Chem model. Concentrations of ammonia throughout California, sulfur dioxide (SO[subscript 2]) in the Central Valley, and ammonium nitrate in the Los Angeles (LA) area are underestimated several-fold in the model. We find that model concentrations are relatively insensitive to uncertainties in gas-particle partitioning and deposition processes in the region. Conversely, increases to anthropogenic livestock ammonia emissions (by a factor of 5) and anthropogenic sulfur dioxide emissions in the Central Valley (by a factor of 3–10) and a reduction of anthropogenic NO[subscript x] emissions (by 30%) substantially reduce the bias in the simulation of gases (SO[subscript 2], NH[subscript 2], HNO[subscript 2]) throughout California and PM[subscript 2.5] near LA, although the exact magnitudes of emissions in the region remain uncertain. Using these modified emissions, we investigate year-round PM[subscript 2.5] air quality in California. The model reproduces the wintertime maximum in surface ammonium nitrate concentrations in the Central Valley (regional mean concentrations are three times higher in December than in June), associated with lower planetary boundary layer heights and colder temperatures, and the wintertime minimum in the LA region (regional mean concentrations are two times higher in June than December) associated with ammonia limitation. Year round, we attribute at least 50% of the inorganic PM[subscript 2.5] mass simulated throughout California to anthropogenic ammonia emissions.en_US
dc.description.sponsorshipUnited States. National Oceanic and Atmospheric Administration (NOAA grant NA12OAR4310064)en_US
dc.description.sponsorshipUnited States. Environmental Protection Agency (EPA STAR Program)en_US
dc.description.sponsorshipUnited States. Environmental Protection Agency (cooperative agreement (GAD R83374))en_US
dc.language.isoen_US
dc.publisherJohn Wiley & Sons, Inc/American Geophysical Unionen_US
dc.relation.isversionofhttp://dx.doi.org/10.1002/2013jd020765en_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.titleAn investigation of ammonia and inorganic particulate matter in California during the CalNex campaignen_US
dc.typeArticleen_US
dc.identifier.citationSchiferl, Luke D., Colette L. Heald, John B. Nowak, John S. Holloway, J. Andrew Neuman, Roya Bahreini, Ilana B. Pollack, Thomas B. Ryerson, Christine Wiedinmyer, and Jennifer G. Murphy. “An Investigation of Ammonia and Inorganic Particulate Matter in California During the CalNex Campaign.” Journal of Geophysical Research: Atmospheres 119, no. 4 (February 24, 2014): 1883–1902. ©2014 American Geophysical Union.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.mitauthorSchiferl, Luke Danielen_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.orderedauthorsSchiferl, Luke D.; Heald, Colette L.; Nowak, John B.; Holloway, John S.; Neuman, J. Andrew; Bahreini, Roya; Pollack, Ilana B.; Ryerson, Thomas B.; Wiedinmyer, Christine; Murphy, Jennifer G.en_US
dc.identifier.orcidhttps://orcid.org/0000-0003-2894-5738
dc.identifier.orcidhttps://orcid.org/0000-0002-5047-2490
mit.licensePUBLISHER_POLICYen_US
mit.metadata.statusComplete


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