Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/106356
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dc.contributorDepartment of Mechanical Engineeringen_US
dc.creatorShen, Jen_US
dc.creatorYu, Men_US
dc.creatorChan, TLen_US
dc.creatorTu, Cen_US
dc.creatorLiu, Yen_US
dc.date.accessioned2024-05-09T00:52:58Z-
dc.date.available2024-05-09T00:52:58Z-
dc.identifier.issn2169-9275en_US
dc.identifier.urihttp://hdl.handle.net/10397/106356-
dc.language.isoenen_US
dc.publisherWiley-Blackwell Publishing, Inc.en_US
dc.rights© 2020. American Geophysical Union. All Rights Reserved.en_US
dc.titleEfficient method of moments for simulating atmospheric aerosol growth : model description, verification, and applicationen_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.volume125en_US
dc.identifier.issue13en_US
dc.identifier.doi10.1029/2019JD032172en_US
dcterms.abstractThe atmospheric aerosol dynamics model (AADM) has been widely used in both comprehensive air quality model systems and chemical transport modeling globally. The AADM consists of Smoluchowski's coagulation equation (SCE), whose solution undergoing Brownian coagulation in the free molecular regime is a challenge because it is inconsistent with aerosols whose size distribution cannot exactly follow the lognormal size distribution. Thus, a new method for solving the SCE without assuming lognormal size distribution is proposed and developed. The underlying principle of this method is that the hybridization of the well-established method of moments with the assumed lognormal size distribution (log MOM) and Taylor-series expansion method of moments (TEMOM) is implemented. This method shows excellent agreement with the sectional method (SM) which is used as reference. The accuracy of these two specific models closely approaches that of the TEMOM, but overcomes the limitation of the classical log MOM. The computational time of this scheme is considerably lower than that of the SM. The new method was successfully implemented to reveal the formation and growth of secondary particles emitted from a vehicle exhaust tailpipe. It was found that the formation of new particles only occurs in the interface region of the turbulent exhaust jet (which is very close to the tailpipe exit), whereas no new particles are formed in the mixture of the exhaust jet plume and the surrounding cold air downstream. The new method is verified as an efficient and reliable numerical scheme for studying atmospheric aerosol dynamics.en_US
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationJournal of geophysical research: oceans, 16 July 2020, v. 125, no. 13, e2019JD032172en_US
dcterms.isPartOfJournal of geophysical research: oceansen_US
dcterms.issued2020-07-16-
dc.identifier.scopus2-s2.0-85087734038-
dc.identifier.eissn2169-9291en_US
dc.identifier.artne2019JD032172en_US
dc.description.validate202405 bcchen_US
dc.description.oaVersion of Recorden_US
dc.identifier.FolderNumberME-0230-
dc.description.fundingSourceOthersen_US
dc.description.fundingTextZhejiang Provincial Natural Science Foundation of China; National Natural Science Foundation of Chinaen_US
dc.description.pubStatusPublisheden_US
dc.identifier.OPUS42884225-
dc.description.oaCategoryVoR alloweden_US
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