Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/111320
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dc.contributorDepartment of Civil and Environmental Engineeringen_US
dc.creatorZhang, Yen_US
dc.creatorChen, Xen_US
dc.creatorWang, Ten_US
dc.creatorLi, Qen_US
dc.creatorXia, Men_US
dc.creatorLi, Men_US
dc.creatorMu, Jen_US
dc.creatorShen, Hen_US
dc.creatorHerrmann, Hen_US
dc.creatorXue, Len_US
dc.date.accessioned2025-02-17T07:03:55Z-
dc.date.available2025-02-17T07:03:55Z-
dc.identifier.issn2169-897Xen_US
dc.identifier.urihttp://hdl.handle.net/10397/111320-
dc.language.isoenen_US
dc.publisherWiley-Blackwell Publishing, Inc.en_US
dc.rights© 2024. American Geophysical Union. All Rights Reserved.en_US
dc.titleDual role of aerosols on reactive bromine recycling in extrapolar marine and continental regionsen_US
dc.typeJournal/Magazine Articleen_US
dc.description.otherinformationTitle on author's file: Dual Role of Aerosols on Reactive Bromine Recycling in Extra-Polar Marine and Continental Regionsen_US
dc.identifier.volume129en_US
dc.identifier.issue23en_US
dc.identifier.doi10.1029/2024JD042040en_US
dcterms.abstractReactive bromine species play important roles in atmospheric chemistry and influence the abundance of climate- and air quality-relevant trace gases. While extensive studies have focused on bromine chemistry in polar regions, the bromine species in extrapolar regions, particularly regarding pollution-related bromine recycling, have received less attention. In this study, we examine the factors influencing the bromine recycling at a clean marine site of the North Atlantic (Cape Verde, CVAO), a semipolluted coastal site of the South China Sea (Hok Tsui, HT), and a polluted continental site of North China (Wangdu, WD), using an observation-based model combined with updated halogen chemistry. Our results indicate that aerosol-related multiphase processes significantly affect bromine recycling in these extrapolar sites. Nitrate photodissociation efficiently recycled bromide into the gas phase in regions characterized by strong aerosol acidity (HT) or high aerosol concentrations (WD). Concurrently, bromine species are lost from the gas phase toward aerosol surfaces, with this process being more effective at higher liquid water content (WD > HT > CVAO). In semipolluted and polluted sites, the aerosol-related processes resulted in elevated bromine levels in the daytime compared to nighttime, leading to larger effects of bromine species on ozone than previously thought. Our study suggests the need for a better understanding of the complex effects of aerosols on reactive halogen chemistry.en_US
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationJournal of geophysical research. Atmospheres, 16 Dec. 2024, v. 129, no. 23, e2024JD042040en_US
dcterms.isPartOfJournal of geophysical research. Atmospheresen_US
dcterms.issued2024-12-16-
dc.identifier.eissn2169-8996en_US
dc.identifier.artne2024JD042040en_US
dc.description.validate202502 bcchen_US
dc.description.oaVersion of Recorden_US
dc.identifier.FolderNumbera3405-n01-
dc.description.fundingSourceRGCen_US
dc.description.fundingSourceOthersen_US
dc.description.fundingTextNational Natural Science Foundation of China, China; Hong Kong Polytechnic University, Chinaen_US
dc.description.pubStatusPublisheden_US
dc.description.oaCategoryVoR alloweden_US
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