Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/97989
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dc.contributorDepartment of Civil and Environmental Engineeringen_US
dc.creatorLiu, Yen_US
dc.creatorWang, Ten_US
dc.creatorStavrakou, Ten_US
dc.creatorElguindi, Nen_US
dc.creatorDoumbia, Ten_US
dc.creatorGranier, Cen_US
dc.creatorBouarar, Ien_US
dc.creatorGaubert, Ben_US
dc.creatorBrasseur, GPen_US
dc.date.accessioned2023-04-06T07:18:04Z-
dc.date.available2023-04-06T07:18:04Z-
dc.identifier.issn0048-9697en_US
dc.identifier.urihttp://hdl.handle.net/10397/97989-
dc.language.isoenen_US
dc.publisherElsevieren_US
dc.rights© 2021 Elsevier B.V. All rights reserved.en_US
dc.rights© 2021. This manuscript version is made available under the CC-BY-NC-ND 4.0 license http://creativecommons.org/licenses/by-nc-nd/4.0/.en_US
dc.rightsThe following publication Liu, Y., et al. (2021). "Diverse response of surface ozone to COVID-19 lockdown in China." Science of The Total Environment 789: 147739 is available at https://dx.doi.org/10.1016/j.scitotenv.2021.147739.en_US
dc.subjectCOVID-19en_US
dc.subjectEmission reductionen_US
dc.subjectMeteorological conditionen_US
dc.subjectSurface ozoneen_US
dc.titleDiverse response of surface ozone to COVID-19 lockdown in Chinaen_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.volume789en_US
dc.identifier.doi10.1016/j.scitotenv.2021.147739en_US
dcterms.abstractOzone (O3) is a key oxidant and pollutant in the lower atmosphere. Significant increases in surface O3 have been reported in many cities during the COVID-19 lockdown. Here we conduct comprehensive observation and modeling analyses of surface O3 across China for periods before and during the lockdown. We find that daytime O3 decreased in the subtropical south, in contrast to increases in most other regions. Meteorological changes and emission reductions both contributed to the O3 changes, with a larger impact from the former especially in central China. The plunge in nitrogen oxide (NOx) emission contributed to O3 increases in populated regions, whereas the reduction in volatile organic compounds (VOC) contributed to O3 decreases across the country. Due to a decreasing level of NOx saturation from north to south, the emission reduction in NOx (46%) and VOC (32%) contributed to net O3 increases in north China; the opposite effects of NOx decrease (49%) and VOC decrease (24%) balanced out in central China, whereas the comparable decreases (45–55%) in these two precursors contributed to net O3 declines in south China. Our study highlights the complex dependence of O3 on its precursors and the importance of meteorology in the short-term O3 variability.en_US
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationScience of the total environment, 1 Oct. 2021, v. 789, 147739en_US
dcterms.isPartOfScience of the total environmenten_US
dcterms.issued2021-10-01-
dc.identifier.scopus2-s2.0-85107683747-
dc.identifier.eissn1879-1026en_US
dc.identifier.artn147739en_US
dc.description.validate202303 bcfcen_US
dc.description.oaAccepted Manuscripten_US
dc.identifier.FolderNumberCEE-0132-
dc.description.fundingSourceRGCen_US
dc.description.fundingSourceOthersen_US
dc.description.fundingTextNNSFCen_US
dc.description.pubStatusPublisheden_US
dc.identifier.OPUS52820279-
dc.description.oaCategoryGreen (AAM)en_US
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