Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/115898
DC FieldValueLanguage
dc.contributorDepartment of Land Surveying and Geo-Informatics-
dc.contributorResearch Institute for Sustainable Urban Development-
dc.contributorResearch Institute of Land and Space-
dc.creatorLi, J-
dc.creatorJin, J-
dc.creatorWong, MS-
dc.creatorWang, J-
dc.creatorLee, KH-
dc.creatorQin, K-
dc.creatorChan, PW-
dc.date.accessioned2025-11-13T00:47:52Z-
dc.date.available2025-11-13T00:47:52Z-
dc.identifier.issn1352-2310-
dc.identifier.urihttp://hdl.handle.net/10397/115898-
dc.language.isoenen_US
dc.publisherPergamon Pressen_US
dc.subjectAERONETen_US
dc.subjectAerosol vertical extinction profileen_US
dc.subjectLunar AODen_US
dc.subjectNighttime aerosolen_US
dc.subjectVertical aerosol type distributionen_US
dc.titleUnraveling urban nighttime aerosol characteristics and meteorological factors on AOD-PM relationships in East Asiaen_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.volume360-
dc.identifier.doi10.1016/j.atmosenv.2025.121388-
dcterms.abstractThis study comprehensively investigates nighttime aerosol characteristics across East Asia, addressing a critical gap in current research, as most existing studies focus exclusively on daytime conditions. It systematically examines variations in column-integrated optical properties, vertically resolved extinction profiles, and aerosol-type distributions in six representative regions of East Asia, including Mongolia (MG), Beijing (BJ), Korea (KR), Japan (JP), Hong Kong (HK), and Taiwan (TW). Significant regional differences were identified, with northern regions (MG, BJ, KR, and JP) displaying consistent day-night aerosol optical depth (AOD) and Ångström exponent values. In contrast, southern regions (HK and TW) exhibit pronounced discrepancies. All regions exhibit smoother nighttime extinction profiles than during the daytime. However, northern regions showed sharper vertical decay, while southern regions exhibited secondary peaks attributed to transported smoke aerosols. Additionally, CALIPSO revealed peaks of vertical aerosol distribution at nighttime compared to daytime. Such abnormal phenomenon was then proved to be the more sensitivity of nighttime Lidar signal to upper thin aerosol layers. After removing this bias, the vertical distribution of aerosol types at nighttime is found to be generally consistent with that during the daytime. Meteorological analysis in BJ suggests consistency in AOD-PM relationships between day and night, highlighting temperature as the dominant factor driving seasonal variations in AOD–PM2.5 correlations, followed by relative humidity. The findings provide valuable insights into nighttime aerosol characteristics, supporting future research on diurnal aerosol radiative forcing.-
dcterms.accessRightsembargoed accessen_US
dcterms.bibliographicCitationAtmospheric environment, 1 Nov. 2025, v. 360, 121388-
dcterms.isPartOfAtmospheric environment-
dcterms.issued2025-11-01-
dc.identifier.scopus2-s2.0-105010117241-
dc.identifier.eissn1873-2844-
dc.identifier.artn121388-
dc.description.validate202511 bchy-
dc.description.oaNot applicableen_US
dc.identifier.SubFormIDG000349/2025-08en_US
dc.description.fundingSourceRGCen_US
dc.description.fundingSourceOthersen_US
dc.description.fundingTextThis project is substantially funded by the General Research Fund (Grant No. 15603923 and 15609421), and the Collaborative Research Fund (Grant No. C5062\u201321GF) and Young Collaborative Research Fund (Grant No. C6003\u201322Y) from the Research Grants Council, Hong Kong, China. The authors acknowledge the funding support (Grant No. BBG2 and CD81) from the Research Institute for Sustainable Urban Development, Research Institute of Land and Space, The Hong Kong Polytechnic University, Kowloon, Hong Kong, China. Jun Wang's participation of work is made possible via in-kind support through the Lichtenberger Family Chair professorship in Chemical Engineering in the University of Iowa. We thank the National Aeronautics and Space Administration (NASA) for providing CALIPSO and AERONET products. Thanks are also given to the European Centre for Medium-Range Weather Forest (ECMWF) for providing ERA5 reanalysis data and the China National Environmental Monitoring Center for offering the PM2.5 and PM10 data.en_US
dc.description.pubStatusPublisheden_US
dc.date.embargo2027-11-01en_US
dc.description.oaCategoryGreen (AAM)en_US
Appears in Collections:Journal/Magazine Article
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Embargo End Date 2027-11-01
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