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dc.contributor.authorJia, Mengwei
dc.contributor.authorEvangeliou, Nikolaos
dc.contributor.authorEckhardt, Sabine
dc.contributor.authorHuang, Xin
dc.contributor.authorGao, Jian
dc.contributor.authorDing, Aijun
dc.contributor.authorStohl, Andreas
dc.date.accessioned2021-08-17T09:22:38Z
dc.date.available2021-08-17T09:22:38Z
dc.date.created2021-08-05T14:20:35Z
dc.date.issued2021
dc.identifier.citationGeophysical Research Letters. 2021, 48, e2021GL093243.en_US
dc.identifier.issn0094-8276
dc.identifier.urihttps://hdl.handle.net/11250/2768740
dc.description.abstractDuring the Lunar New Year Holiday of 2020, China implemented an unprecedented lockdown to fight the COVID-19 outbreak, which strongly affected the anthropogenic emissions. We utilized elemental carbon observations (equivalent to black carbon, BC) from 42 sites and performed inverse modeling to determine the impact of the lockdown on the weekly BC emissions and quantify the effect of the stagnant conditions on BC observations in densely populated eastern and northern China. BC emissions declined 70% (eastern China) and 48% (northern China) compared to the first half of January. In northern China, under the stagnant conditions of the first week of the lockdown, the observed BC concentrations rose unexpectedly (29%) even though the BC emissions fell. The emissions declined substantially thereafter until a week after the lockdown ended. On the contrary, in eastern China, BC emissions dropped sharply in the first week and recovered synchronously with the end of the lockdown.en_US
dc.language.isoengen_US
dc.titleBlack Carbon Emission Reduction Due to COVID-19 Lockdown in Chinaen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.rights.holder© 2021. American Geophysical Union. All Rights Reserved.en_US
dc.source.pagenumber10en_US
dc.source.volume48en_US
dc.source.journalGeophysical Research Lettersen_US
dc.source.issue8en_US
dc.identifier.doi10.1029/2021GL093243
dc.identifier.cristin1924161
dc.relation.projectNorges forskningsråd: 275407en_US
dc.source.articlenumbere2021GL093243en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode2


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