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dc.contributor.authorKim, JY-
dc.contributor.authorSong, CH-
dc.contributor.authorGhim, YS-
dc.contributor.authorWon, JG-
dc.contributor.authorYoon, SC-
dc.contributor.authorCarmichael, GR-
dc.contributor.authorWoo, JH-
dc.date.accessioned2024-01-21T03:31:02Z-
dc.date.available2024-01-21T03:31:02Z-
dc.date.created2021-09-01-
dc.date.issued2006-04-
dc.identifier.issn1352-2310-
dc.identifier.urihttps://pubs.kist.re.kr/handle/201004/135624-
dc.description.abstractIn this study, the accuracy of NH3 emissions in East Asia is evaluated by a comparison of measured and predicted NH4NO3 concentrations. For the prediction of particulate NH4NO3 concentrations, this study uses the USEPA Models-3/Community Multi-scale Air Quality (Models-3/CMAQ) model. The measurement data are collected from 4 ground-based stations (Beijing, Shanghai, Qingdao, and Kangwha) and ACE-ASIA C130 Flights #6, #7, and #10. The four ground-based stations and air flight tracks are located in and around the Yellow Sea in East Asia. According to the results, the predicted fine-mode NH4+ concentrations are 1.2-3.8 times overestimated compared to those measured on the mass basis, and fine-mode NO3- concentrations are 1.9-7.6 times overestimated on the mass basis. It is also revealed in this study that aberrantly high predicted fine-mode NO3- concentrations in East Asia can be attributed to the overestimated NH3 emissions. The predicted gas-phase NH3 concentrations and estimated NH3 emissions are likely to be 1.2-3.8 times overestimated in East Asia on the mass basis. Therefore, it is recommended that approximately 20-75% reduced NH3 emission fields should be used in future modeling studies for East Asia. (c) 2005 Elsevier Ltd. All rights reserved.-
dc.languageEnglish-
dc.publisherPERGAMON-ELSEVIER SCIENCE LTD-
dc.subjectEQUILIBRIUM-MODEL-
dc.subjectDEPOSITION-
dc.subjectNITRATE-
dc.subjectPARTICLES-
dc.subjectINVENTORY-
dc.subjectEVOLUTION-
dc.subjectSULFATE-
dc.subjectPM2.5-
dc.titleAn investigation on NH3 emissions and particulate NH4+-NO3- formation in East Asia-
dc.typeArticle-
dc.identifier.doi10.1016/j.atmosenv.2005.11.048-
dc.description.journalClass1-
dc.identifier.bibliographicCitationATMOSPHERIC ENVIRONMENT, v.40, no.12, pp.2139 - 2150-
dc.citation.titleATMOSPHERIC ENVIRONMENT-
dc.citation.volume40-
dc.citation.number12-
dc.citation.startPage2139-
dc.citation.endPage2150-
dc.description.journalRegisteredClassscie-
dc.description.journalRegisteredClassscopus-
dc.identifier.wosid000236527700006-
dc.identifier.scopusid2-s2.0-32844468671-
dc.relation.journalWebOfScienceCategoryEnvironmental Sciences-
dc.relation.journalWebOfScienceCategoryMeteorology & Atmospheric Sciences-
dc.relation.journalResearchAreaEnvironmental Sciences & Ecology-
dc.relation.journalResearchAreaMeteorology & Atmospheric Sciences-
dc.type.docTypeArticle-
dc.subject.keywordPlusEQUILIBRIUM-MODEL-
dc.subject.keywordPlusDEPOSITION-
dc.subject.keywordPlusNITRATE-
dc.subject.keywordPlusPARTICLES-
dc.subject.keywordPlusINVENTORY-
dc.subject.keywordPlusEVOLUTION-
dc.subject.keywordPlusSULFATE-
dc.subject.keywordPlusPM2.5-
dc.subject.keywordAuthorNH3 emissions-
dc.subject.keywordAuthorNH4NO3 formation-
dc.subject.keywordAuthorModels-3/CMAQ model-
dc.subject.keywordAuthorEast Asia-
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