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dc.contributor.authorSkeie, Ragnhild Bieltvedt
dc.contributor.authorByrom, Rachael
dc.contributor.authorHodnebrog, Øivind
dc.contributor.authorJouan, Caroline
dc.contributor.authorMyhre, Gunnar
dc.date.accessioned2025-01-27T11:29:03Z
dc.date.available2025-01-27T11:29:03Z
dc.date.created2025-01-13T09:09:39Z
dc.date.issued2024
dc.identifier.citationAtmospheric Chemistry and Physics (ACP). 2024, 24 (23), 13361-13370.en_US
dc.identifier.issn1680-7316
dc.identifier.urihttps://hdl.handle.net/11250/3174514
dc.description.abstractNew regulations of sulfur emissions from shipping were introduced in 2020, reducing emissions of SO2 from international shipping by ∼ 80 %. As SO2 is an aerosol precursor, this drop in emissions over the ocean will weaken the total aerosol effective radiative forcing (ERF) that has historically masked an uncertain fraction of the warming due to the increased concentration of greenhouse gases in the atmosphere. Here, we use four global climate models and a chemical transport model to calculate the ERF resulting from an 80 % reduction in SO2 emissions from international shipping relative to 2019 emission estimates. The individual model means range from 0.06 to 0.09 W m−2, corresponding to the ERF resulting from the increase in CO2 concentration over the last 2 to 3 years. The full uncertainty in the ERF due to the new regulation is not quantified but will very likely be high considering the contribution of uncertainties in shipping SO2 emissions, the sulfur cycle, the modelling of cloud adjustments and the impact of interannual variability on the method for calculating radiative forcing.en_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.titleMulti-model effective radiative forcing of the 2020 sulfur cap for shippingen_US
dc.title.alternativeMulti-model effective radiative forcing of the 2020 sulfur cap for shippingen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.source.pagenumber13361-13370en_US
dc.source.volume24en_US
dc.source.journalAtmospheric Chemistry and Physics (ACP)en_US
dc.source.issue23en_US
dc.identifier.doi10.5194/acp-24-13361-2024
dc.identifier.cristin2339515
dc.relation.projectNorges forskningsråd: 314997en_US
dc.relation.projectEC/H2020/820829en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode2


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