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dc.contributor.authorMyhre, Gunnar
dc.contributor.authorSamset, Bjørn Hallvard
dc.contributor.authorMohr, Christian Wilhelm
dc.contributor.authorAlterskjær, Kari
dc.contributor.authorBalkanski, Yves
dc.contributor.authorBellouin, Nicolas
dc.contributor.authorChin, Mian
dc.contributor.authorHaywood, James
dc.contributor.authorHodnebrog, Øivind
dc.contributor.authorKinne, Stefan
dc.contributor.authorLin, Guangxing
dc.contributor.authorLund, Marianne Tronstad
dc.contributor.authorPenner, Joyce E.
dc.contributor.authorSchulz, Michael
dc.contributor.authorSchutgens, Nick
dc.contributor.authorSkeie, Ragnhild Bieltvedt
dc.contributor.authorStier, Philip
dc.contributor.authorTakemura, Toshihiko
dc.contributor.authorZhang, Kai
dc.date.accessioned2021-08-24T09:27:26Z
dc.date.available2021-08-24T09:27:26Z
dc.date.created2020-09-29T20:15:59Z
dc.date.issued2020
dc.identifier.citationAtmospheric Chemistry and Physics. 2020, 20 8855-8865.en_US
dc.identifier.issn1680-7316
dc.identifier.urihttps://hdl.handle.net/11250/2770912
dc.description.abstractThe radiative forcing of the aerosol–radiation interaction can be decomposed into clear-sky and cloudy-sky portions. Two sets of multi-model simulations within Aerosol Comparisons between Observations and Models (AeroCom), combined with observational methods, and the time evolution of aerosol emissions over the industrial era show that the contribution from cloudy-sky regions is likely weak. A mean of the simulations considered is 0.01±0.1 W m−2. Multivariate data analysis of results from AeroCom Phase II shows that many factors influence the strength of the cloudy-sky contribution to the forcing of the aerosol–radiation interaction. Overall, single-scattering albedo of anthropogenic aerosols and the interaction of aerosols with the short-wave cloud radiative effects are found to be important factors. A more dedicated focus on the contribution from the cloud-free and cloud-covered sky fraction, respectively, to the aerosol–radiation interaction will benefit the quantification of the radiative forcing and its uncertainty range.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.titleCloudy-sky contributions to the direct aerosol effecten_US
dc.typeJournal articleen_US
dc.typePeer revieweden_US
dc.description.versionpublishedVersionen_US
dc.source.pagenumber8855-8865en_US
dc.source.volume20en_US
dc.source.journalAtmospheric Chemistry and Physicsen_US
dc.identifier.doi10.5194/acp-20-8855-2020
dc.identifier.cristin1835170
dc.relation.projectNorges forskningsråd: 295046en_US
dc.relation.projectNotur/NorStore: NS9252Ken_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode2


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Navngivelse 4.0 Internasjonal
Except where otherwise noted, this item's license is described as Navngivelse 4.0 Internasjonal