Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/23156
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dc.contributorDepartment of Civil and Environmental Engineering-
dc.creatorZhou, D-
dc.creatorDing, A-
dc.creatorMao, H-
dc.creatorFu, C-
dc.creatorWang, T-
dc.creatorChan, LY-
dc.creatorDing, K-
dc.creatorZhang, Y-
dc.creatorLiu, J-
dc.creatorLu, A-
dc.creatorHao, N-
dc.date.accessioned2014-12-31T08:02:44Z-
dc.date.available2014-12-31T08:02:44Z-
dc.identifier.issn1748-9318en_US
dc.identifier.urihttp://hdl.handle.net/10397/23156-
dc.language.isoenen_US
dc.publisherInstitute of Physics Publishingen_US
dc.rights© 2013 IOP Publishing Ltd. Content from this work may be used under the terms of the Creative Commons Attribution 3.0 licence. Any further distribution of this work must maintain attribution to the author(s) and the title of the work, journal citation and DOI.en_US
dc.rightsThe following publication Zhou, D., Ding, A., Mao, H., Fu, C., Wang, T., Chan, L. Y., ... & Hao, N. (2013). Impacts of the East Asian monsoon on lower tropospheric ozone over coastal South China. Environmental Research Letters, 8(4), 044011 is available at https://doi.org/10.1088/1748-9326/8/4/044011en_US
dc.subjectAsian monsoonen_US
dc.subjectClimatologyen_US
dc.subjectInterannual variabilityen_US
dc.subjectTropospheric ozoneen_US
dc.titleImpacts of the East Asian monsoon on lower tropospheric ozone over coastal South Chinaen_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.volume8en_US
dc.identifier.issue4en_US
dc.identifier.doi10.1088/1748-9326/8/4/044011en_US
dcterms.abstractThe impact of the East Asian monsoon (EAM) on climatology and interannual variability of tropospheric ozone (O3) over the coastal South China was investigated by analyzing 11 years of ozonesonde data over Hong Kong with the aid of Lagrangian dispersion modeling of carbon monoxide and calculation of an EAM index. It was found that the seasonal cycle of O3 in the lower troposphere is highly related to the EAM over the study region. Ozone enhancements in the free troposphere are associated with the monsoon-induced transport of pollutants of continental anthropogenic and biomass burning origins. Lower tropospheric O3 levels showed high interannual variability, with an annual averaged amplitude up to 61% of averaged concentrations in the boundary layer (0-1 km altitudes) and 49% below 3 km altitude. In spring and autumn, the interannual variability in boundary layer O3 levels was predominately influenced by the EAM intensity, with high O3 mixing ratios associated with northeasterly circulation anomalies.-
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationEnvironmental research letters, 2013, v. 8, no. 4, 044011-
dcterms.isPartOfEnvironmental research letters-
dcterms.issued2013-
dc.identifier.scopus2-s2.0-84891926885-
dc.identifier.eissn1748-9326en_US
dc.identifier.rosgroupidr71199-
dc.description.ros2013-2014 > Academic research: refereed > Publication in refereed journalen_US
dc.description.validate201901_a bcmaen_US
dc.description.oaVersion of Recorden_US
dc.identifier.FolderNumberOA_IR/PIRAen_US
dc.description.pubStatusPublisheden_US
dc.description.oaCategoryCCen_US
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