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dc.contributor.authorAhsan, Hamza
dc.contributor.authorWang, Hailong
dc.contributor.authorWu, Jingbo
dc.contributor.authorWu, Mingxuan
dc.contributor.authorSmith, Steven J.
dc.contributor.authorBauer, Susanne
dc.contributor.authorSuchyta, Harrison
dc.contributor.authorOliviè, Dirk Jan Leo
dc.contributor.authorMyhre, Gunnar
dc.contributor.authorMatsui, Hitoshi
dc.contributor.authorBian, Huisheng
dc.contributor.authorLamarque, Jean-François
dc.contributor.authorCarslaw, Ken
dc.contributor.authorHorowitz, Larry
dc.contributor.authorRegayre, Leighton
dc.contributor.authorChin, Mian
dc.contributor.authorSchulz, Michael
dc.contributor.authorSkeie, Ragnhild Bieltvedt
dc.contributor.authorTakemura, Toshihiko
dc.contributor.authorNaik, Vaishali
dc.date.accessioned2024-03-18T13:12:10Z
dc.date.available2024-03-18T13:12:10Z
dc.date.created2024-01-02T10:05:19Z
dc.date.issued2023
dc.identifier.citationAtmospheric Chemistry and Physics (ACP). 2023, 23 (23), 14779-14799.en_US
dc.identifier.issn1680-7316
dc.identifier.urihttps://hdl.handle.net/11250/3122915
dc.description.abstractAnthropogenic emissions of aerosols and precursor compounds are known to significantly affect the energy balance of the Earth–atmosphere system, alter the formation of clouds and precipitation, and have a substantial impact on human health and the environment. Global models are an essential tool for examining the impacts of these emissions. In this study, we examine the sensitivity of model results to the assumed height of SO2 injection, seasonality of SO2 and black carbon (BC) particulate emissions, and the assumed fraction of SO2 emissions that is injected into the atmosphere as particulate phase sulfate (SO4) in 11 climate and chemistry models, including both chemical transport models and the atmospheric component of Earth system models. We find large variation in atmospheric lifetime across models for SO2, SO4, and BC, with a particularly large relative variation for SO2, which indicates that fundamental aspects of atmospheric sulfur chemistry remain uncertain. Of the perturbations examined in this study, the assumed height of SO2 injection had the largest overall impacts, particularly on global mean net radiative flux (maximum difference of −0.35 W m−2), SO2 lifetime over Northern Hemisphere land (maximum difference of 0.8 d), surface SO2 concentration (up to 59 % decrease), and surface sulfate concentration (up to 23 % increase). Emitting SO2 at height consistently increased SO2 and SO4 column burdens and shortwave cooling, with varying magnitudes, but had inconsistent effects across models on the sign of the change in implied cloud forcing. The assumed SO4 emission fraction also had a significant impact on net radiative flux and surface sulfate concentration. Because these properties are not standardized across models this is a source of inter-model diversity typically neglected in model intercomparisons. These results imply a need to ensure that anthropogenic emission injection height and SO4 emission fraction are accurately and consistently represented in global models.en_US
dc.description.abstractThe Emissions Model Intercomparison Project (Emissions-MIP): Quantifying model sensitivity to emission characteristicsen_US
dc.language.isoengen_US
dc.publisherCopernicus Publicationsen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleThe Emissions Model Intercomparison Project (Emissions-MIP): Quantifying model sensitivity to emission characteristicsen_US
dc.title.alternativeThe Emissions Model Intercomparison Project (Emissions-MIP): Quantifying model sensitivity to emission characteristicsen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.source.pagenumber14779-14799en_US
dc.source.volume23en_US
dc.source.journalAtmospheric Chemistry and Physics (ACP)en_US
dc.source.issue23en_US
dc.identifier.doi10.5194/acp-23-14779-2023
dc.identifier.cristin2218663
dc.relation.projectNorges forskningsråd: 270061en_US
dc.relation.projectNorges forskningsråd: 295046en_US
dc.relation.projectEC/H2020/821205en_US
dc.relation.projectNorges forskningsråd: 314997en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode2


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