Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/111684
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dc.contributorDepartment of Civil and Environmental Engineering-
dc.creatorZhang, Men_US
dc.creatorChen, JMen_US
dc.creatorWang, Ten_US
dc.creatorCheng, TTen_US
dc.creatorLin, Len_US
dc.creatorBhatia, RSen_US
dc.creatorHanvey, Men_US
dc.date.accessioned2025-03-13T02:22:00Z-
dc.date.available2025-03-13T02:22:00Z-
dc.identifier.issn2169-897Xen_US
dc.identifier.urihttp://hdl.handle.net/10397/111684-
dc.language.isoenen_US
dc.publisherWiley-Blackwell Publishing, Inc.en_US
dc.rightsCopyright 2010 by the American Geophysical Union.en_US
dc.titleChemical characterization of aerosols over the Atlantic Ocean and the Pacific Ocean during two cruises in 2007 and 2008en_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.volume115en_US
dc.identifier.issueD22en_US
dc.identifier.doi10.1029/2010JD014246en_US
dcterms.abstract[1] To help understand the chemical properties of marine aerosols and the long-distance transport of continental aerosols to remote oceanic regions, total suspended particulates (TSP) samples were collected over the Atlantic Ocean and the Pacific Ocean during two cruises in September–December 2007 (cruise I) and March–April 2008 (cruise II) aboard the M/V Oceanic II. Data were analyzed and interpreted with the aid of back trajectory, principal component, and multiple linear regression analyses. Compared with the results over the South Pacific from 2 decades ago, the non-sea-salt sulfate (NSS-SO42−) concentrations over the South Pacific have increased by a factor of ∼1.5, while the NO3− concentration has remained constant. On average, NSS-SO42− accounted for 30–52% of the total SO42− during the two cruises. Chloride deficit was observed in all samples, with NSS-SO42− being the preferred species for acid displacement over the South Pacific and the Mediterranean Sea. Persistent clean marine air masses were only observed over the northern Atlantic and South Pacific during cruise I, while more frequent impacts of continental air (dust, biomass burning, and industrial plumes) were observed during cruise II. Combined with the NAAPS aerosol maps, these results indicate that during cruise II, (1) southern Atlantic was influenced by Southern Africa and the interhemisphere transport of biomass burning plumes in Central Africa, (2) northern Atlantic was under the combined pollution plumes of Sahara dust intrusion and biomass burning, and (3) the Mediterranean Sea was affected by the mixed pollution from biomass burning and industrial contamination, as well as Saharan dust.-
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationJournal of geophysical research. Atmospheres, 27 Nov. 2010, v. 115, D22, D22302en_US
dcterms.isPartOfJournal of geophysical research. Atmospheresen_US
dcterms.issued2010-11-27-
dc.identifier.scopus2-s2.0-78649494490-
dc.identifier.eissn2169-8996en_US
dc.identifier.artnD22302en_US
dc.description.validate202503 bcch-
dc.description.oaVersion of Recorden_US
dc.identifier.FolderNumberOA_Others-
dc.description.fundingSourceOthersen_US
dc.description.fundingTextNational Natural Science Foundation of China; Chinese Ministry of Education; Science and Technology Commission of Shanghai Municipality; Royal Caribbean Internationalen_US
dc.description.pubStatusPublisheden_US
dc.description.oaCategoryVoR alloweden_US
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