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dc.contributor.authorYan, Chaoes_ES
dc.contributor.authorTham, Yee Junes_ES
dc.contributor.authorNie, Weies_ES
dc.contributor.authorXia, Menes_ES
dc.contributor.authorWang, Haichaoes_ES
dc.contributor.authorGuo, Yishuoes_ES
dc.contributor.authorMa, Weies_ES
dc.contributor.authorZhan, Junleies_ES
dc.contributor.authorHua, Chenjiees_ES
dc.contributor.authorLi, Yuanyuanes_ES
dc.contributor.authorDeng, Chenjuanes_ES
dc.contributor.authorLi, Yiranes_ES
dc.contributor.authorZheng, Feixuees_ES
dc.contributor.authorChen, Xines_ES
dc.contributor.authorLi, Qinyies_ES
dc.contributor.authorZhang, Genes_ES
dc.contributor.authorMahajan, Anoop S.es_ES
dc.contributor.authorCuevas, Carlos A.es_ES
dc.contributor.authorHuang, Dan Danes_ES
dc.contributor.authorWang, Zhees_ES
dc.contributor.authorSun, Yelees_ES
dc.contributor.authorSaiz-Lopez, A.es_ES
dc.contributor.authorBianchi, Federicoes_ES
dc.contributor.authorKerminen, Veli Matties_ES
dc.contributor.authorWorsnop, Douglas R.es_ES
dc.contributor.authorDonahue, Neil M.es_ES
dc.contributor.authorJiang, Jingkunes_ES
dc.contributor.authorLiu, Yongchunes_ES
dc.contributor.authorDing, Aijunes_ES
dc.contributor.authorKulmala, Markkues_ES
dc.date.accessioned2024-01-30T09:29:01Z-
dc.date.available2024-01-30T09:29:01Z-
dc.date.issued2023-11-01-
dc.identifier.citationNature Geoscience 16: 975–981 (2023)es_ES
dc.identifier.issn1752-0894-
dc.identifier.urihttp://hdl.handle.net/10261/344319-
dc.description.abstractNitrate comprises the largest fraction of fine particulate matter in China during severe haze. Consequently, strict control of nitrogen oxides (NOx) emissions has been regarded as an effective measure to combat air pollution. However, this notion is challenged by the persistent severe haze pollution observed during the COVID-19 lockdown when NOx levels substantially declined. Here we present direct field evidence that diminished nitrogen monoxide (NO) during the lockdown activated nocturnal nitrogen chemistry, driving severe haze formation. First, dinitrogen pentoxide (N2O5) heterogeneous reactions dominate particulate nitrate (pNO3−) formation during severe pollution, explaining the higher-than-normal pNO3− fraction in fine particulate matter despite the substantial NOx reduction. Second, N2O5 heterogeneous reactions provide a large source of chlorine radicals on the following day, contributing drastically to the oxidation of volatile organic compounds, and thus the formation of oxygenated organic molecules and secondary organic aerosol. Our findings highlight the increasing importance of such nocturnal nitrogen chemistry in haze formation caused by NOx reduction, motivating refinements to future air pollution control strategies.es_ES
dc.description.sponsorshipThis work is supported by the National Natural Science Foundation of China (NSFC) project (92044301, 42220104006, 42075101 and 41975154), the Academy of Finland (1251427, 1139656, 296628, 306853, 316114 and 311932), the Finnish Centre of Excellence (1141135 and 307331), the European Union’s Horizon 2020 programme (ERC, project no.742206 ‘ATM-GTP’, no. 850614 ‘CHAPAs’ and no. 895875 ‘NPF-PANDA’), the trans-national ERA-PLANET project SMURBS (project no. 689443) under the EU Horizon 2020 Framework Programme, the European Regional Development Fund, the Urban Innovative Actions initiative (HOPE; Healthy Outdoor Premises for Everyone, project no. UIA03 − 240), MegaSense by Business Finland (grant no. 7517/31/2018) and Academy of Finland Flagship funding (grant no. 337549). The Beijing University of Chemical Technology team is supported by the National Natural Science Foundation of China (42275117) and the Beijing Natural Science Foundation (8232041). Y.J.T. acknowledges the funding support from the National Natural Science Foundation of China (42175118) and the Guangdong Basic and Applied Basic Research Foundation (2022A1515010852). The CSIC team acknowledges the funding support from the European Research Council Executive Agency under the European Union’s Horizon 2020 Research and Innovation Programme (project ERC‐2016‐COG, project no. 726349 CLIMAHAL to A.S.-L.). The Tsinghua University team acknowledges the National Natural Science Foundation of China (22188102) and Samsung PM2.5 SRP. N.M.D. acknowledges the US National Science Foundation grant AGS2132089. H.W. acknowledges the funding support from the National Natural Science Foundation of China (42175111). The Indian Institute of Tropical Meteorology is funded by the Ministry of Earth Sciences, Government of India. We acknowledge the German federal environmental agency for kindly providing us with the O3, NOx and PM2.5 and PM10 data in Frankfurt and Berlin. The data at the Frankfurt sites were measured by Hessisches Landesamt für Naturschutz, Umwelt und Geologie and the data at the Berlin sites were measured by Senatsverwaltung für Umwelt, Mobilität, Verbraucher- und Klimaschutz. We thank them for their great efort. We acknowledge the Madrid Air Quality Monitoring Network, Smart SMEAR Network, India Central Pollution Control Board and California Air Resources Board for the NOx, O3, CO and PM2.5 open data sources.es_ES
dc.language.isoenges_ES
dc.publisherNature Publishing Groupes_ES
dc.relationinfo:eu-repo/grantAgreement/EC/H2020/850614es_ES
dc.relationinfo:eu-repo/grantAgreement/EC/H2020/895875es_ES
dc.relationinfo:eu-repo/grantAgreement/EC/H2020/689443es_ES
dc.relationinfo:eu-repo/grantAgreement/EC/H2020/726349es_ES
dc.relation.ispartofNature Geosciencees_ES
dc.relation.isversionofPostprintes_ES
dc.rightsopenAccessen_EN
dc.titleIncreasing contribution of nighttime nitrogen chemistry to wintertime haze formation in Beijing observed during COVID-19 lockdownses_ES
dc.typeartículoes_ES
dc.identifier.doi10.1038/s41561-023-01285-1-
dc.description.peerreviewedPeer reviewedes_ES
dc.relation.publisherversionhttps://doi.org/10.1038/s41561-023-01285-1es_ES
dc.contributor.funderNational Natural Science Foundation of Chinaes_ES
dc.contributor.funderAcademy of Finlandes_ES
dc.contributor.funderEuropean Commissiones_ES
dc.contributor.funderBeijing University of Chemical Technologyes_ES
dc.contributor.funderBasic and Applied Basic Foundation of Guangdong Provincees_ES
dc.contributor.funderConsejo Superior de Investigaciones Científicas (España)es_ES
dc.contributor.funderTsinghua Universityes_ES
dc.contributor.funderNational Science Foundation (US)es_ES
dc.contributor.funderIndian Institute of Tropical Meteorologyes_ES
dc.contributor.funderMinistry of Earth Sciences (India)es_ES
dc.contributor.funderGerman Federal Environmental Foundationes_ES
dc.relation.csices_ES
oprm.item.hasRevisionno ko 0 false*
dc.identifier.funderhttp://dx.doi.org/10.13039/501100001851es_ES
dc.identifier.funderhttp://dx.doi.org/10.13039/100000001es_ES
dc.identifier.funderhttp://dx.doi.org/10.13039/501100001809es_ES
dc.identifier.funderhttp://dx.doi.org/10.13039/100007636es_ES
dc.identifier.funderhttp://dx.doi.org/10.13039/501100002341es_ES
dc.identifier.funderhttp://dx.doi.org/10.13039/501100007302es_ES
dc.identifier.funderhttp://dx.doi.org/10.13039/501100000780es_ES
dc.identifier.funderhttp://dx.doi.org/10.13039/501100004147es_ES
dc.identifier.funderhttp://dx.doi.org/10.13039/501100003339es_ES
dc.contributor.orcidYan, Chao [0000-0002-5735-9597]es_ES
dc.contributor.orcidTham, Yee Jun [0000-0001-7924-5841]es_ES
dc.contributor.orcidNie, Wei [0000-0002-6048-0515]es_ES
dc.contributor.orcidXia, Men [0000-0002-8534-3357]es_ES
dc.contributor.orcidWang, Haichao [0000-0001-6161-1874]es_ES
dc.contributor.orcidMa, Wei [0000-0001-8975-1764]es_ES
dc.contributor.orcidZhan, Junlei [0000-0002-5968-9370]es_ES
dc.contributor.orcidLi, Yiran [0000-0001-7232-4969]es_ES
dc.contributor.orcidLi, Qinyi [0000-0002-5146-5831]es_ES
dc.contributor.orcidMahajan, Anoop S. [0000-0002-2909-5432]es_ES
dc.contributor.orcidCuevas, Carlos A. [0000-0002-9251-5460]es_ES
dc.contributor.orcidWang, Zhe [0000-0002-5627-6562]es_ES
dc.contributor.orcidSun, Yele [0000-0003-2354-0221]es_ES
dc.contributor.orcidSaiz-Lopez, A. [0000-0002-0060-1581]es_ES
dc.contributor.orcidBianchi, Federico [0000-0003-2996-3604]es_ES
dc.contributor.orcidKerminen, Veli Matti [0000-0002-0706-669X]es_ES
dc.contributor.orcidWorsnop, Douglas R. [0000-0002-8928-8017]es_ES
dc.contributor.orcidDonahue, Neil M. [0000-0003-3054-2364]es_ES
dc.contributor.orcidLiu, Yongchun [0000-0002-9055-970X]es_ES
dc.contributor.orcidDing, Aijun [0000-0003-4481-5386]es_ES
dc.contributor.orcidKulmala, Markku [0000-0003-3464-7825]es_ES
dc.identifier.scopus2-s2.0-85174063846-
dc.identifier.urlhttps://api.elsevier.com/content/abstract/scopus_id/85174063846-
dc.type.coarhttp://purl.org/coar/resource_type/c_6501es_ES
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item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.languageiso639-1en-
item.cerifentitytypePublications-
item.openairetypeartículo-
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