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dc.contributor.authorWhaley, Cynthia
dc.contributor.authorMahmood, Rashed
dc.contributor.authorvon Salzen, Knut
dc.contributor.authorWinter, Barbara
dc.contributor.authorEckhardt, Sabine
dc.contributor.authorArnold, Stephen R.
dc.contributor.authorBeagley, Stephen
dc.contributor.authorBecagli, Silvia
dc.contributor.authorChien, Rong-You
dc.contributor.authorChristensen, Jesper
dc.contributor.authorDamani, Sujay Manish
dc.contributor.authorDong, Xinyi
dc.contributor.authorEleftheriadis, Konstantinos
dc.contributor.authorEvangeliou, Nikolaos
dc.contributor.authorFaluvegi, Gregory
dc.contributor.authorFlanner, Mark G.
dc.contributor.authorFu, Joshua S.
dc.contributor.authorGauss, Michael
dc.contributor.authorGiardi, Fabio
dc.contributor.authorGong, Wanmin
dc.contributor.authorHjorth, Jens Liengaard
dc.contributor.authorHuang, Lin
dc.contributor.authorIm, Ulas
dc.contributor.authorKanaya, Yugo
dc.contributor.authorSrinath, Krishnan
dc.contributor.authorKlimont, Zbigniew
dc.contributor.authorKuhn, Thomas
dc.contributor.authorLangner, Joakim
dc.contributor.authorLaw, Kathy S.
dc.contributor.authorMarelle, Louis
dc.contributor.authorMassling, Andreas
dc.contributor.authorOliviè, Dirk Jan Leo
dc.contributor.authorOnishi, Tatsuo
dc.contributor.authorOshima, Naga
dc.contributor.authorPeng, Yiran
dc.contributor.authorPlummer, David A.
dc.contributor.authorPozzoli, Luca
dc.contributor.authorPopovicheva, Olga
dc.contributor.authorRaut, Jean-Christophe
dc.contributor.authorSand, Maria
dc.contributor.authorSaunders, Laura
dc.contributor.authorSchmale, Julia
dc.contributor.authorSharma, Sangeeta
dc.contributor.authorSkeie, Ragnhild Bieltvedt
dc.contributor.authorSkov, Henrik
dc.contributor.authorTaketani, Fumikazu
dc.contributor.authorThomas, Manu Anna
dc.contributor.authorTraversi, Rita
dc.contributor.authorTsigaridis, Kostas
dc.contributor.authorTsyro, Svetlana
dc.contributor.authorTurnock, Steven T
dc.contributor.authorVitale, Vito
dc.contributor.authorWalker, Kaley A.
dc.contributor.authorWang, Minqi
dc.contributor.authorWatson-Parris, Duncan
dc.contributor.authorWeiss-Gibbons, Tahya
dc.date.accessioned2022-06-08T12:00:11Z
dc.date.available2022-06-08T12:00:11Z
dc.date.created2022-05-19T13:25:47Z
dc.date.issued2022
dc.identifier.citationAtmospheric Chemistry and Physics (ACP). 2022, 22 5775-5828.en_US
dc.identifier.issn1680-7316
dc.identifier.urihttps://hdl.handle.net/11250/2997907
dc.description.abstractWhile carbon dioxide is the main cause for global warming, modeling short-lived climate forcers (SLCFs) such as methane, ozone, and particles in the Arctic allows us to simulate near-term climate and health impacts for a sensitive, pristine region that is warming at 3 times the global rate. Atmospheric modeling is critical for understanding the long-range transport of pollutants to the Arctic, as well as the abundance and distribution of SLCFs throughout the Arctic atmosphere. Modeling is also used as a tool to determine SLCF impacts on climate and health in the present and in future emissions scenarios. In this study, we evaluate 18 state-of-the-art atmospheric and Earth system models by assessing their representation of Arctic and Northern Hemisphere atmospheric SLCF distributions, considering a wide range of different chemical species (methane, tropospheric ozone and its precursors, black carbon, sulfate, organic aerosol, and particulate matter) and multiple observational datasets. Model simulations over 4 years (2008–2009 and 2014–2015) conducted for the 2022 Arctic Monitoring and Assessment Programme (AMAP) SLCF assessment report are thoroughly evaluated against satellite, ground, ship, and aircraft-based observations. The annual means, seasonal cycles, and 3-D distributions of SLCFs were evaluated using several metrics, such as absolute and percent model biases and correlation coefficients. The results show a large range in model performance, with no one particular model or model type performing well for all regions and all SLCF species. The multi-model mean (mmm) was able to represent the general features of SLCFs in the Arctic and had the best overall performance. For the SLCFs with the greatest radiative impact (CH4, O3, BC, and SO), the mmm was within ±25 % of the measurements across the Northern Hemisphere. Therefore, we recommend a multi-model ensemble be used for simulating climate and health impacts of SLCFs. Of the SLCFs in our study, model biases were smallest for CH4 and greatest for OA. For most SLCFs, model biases skewed from positive to negative with increasing latitude. Our analysis suggests that vertical mixing, long-range transport, deposition, and wildfires remain highly uncertain processes. These processes need better representation within atmospheric models to improve their simulation of SLCFs in the Arctic environment. As model development proceeds in these areas, we highly recommend that the vertical and 3-D distribution of SLCFs be evaluated, as that information is critical to improving the uncertain processes in models.en_US
dc.description.abstractModel evaluation of short-lived climate forcers for the Arctic Monitoring and Assessment Programme: a multi-species, multi-model studyen_US
dc.language.isoengen_US
dc.publisherEGUen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleModel evaluation of short-lived climate forcers for the Arctic Monitoring and Assessment Programme: a multi-species, multi-model studyen_US
dc.title.alternativeModel evaluation of short-lived climate forcers for the Arctic Monitoring and Assessment Programme: a multi-species, multi-model studyen_US
dc.typeJournal articleen_US
dc.typePeer revieweden_US
dc.description.versionpublishedVersionen_US
dc.source.pagenumber5775-5828en_US
dc.source.volume22en_US
dc.source.journalAtmospheric Chemistry and Physics (ACP)en_US
dc.identifier.doi10.5194/acp-22-5775-2022
dc.identifier.cristin2025633
dc.relation.projectEC/H2020/727890en_US
dc.relation.projectEC/H2020/860100en_US
dc.relation.projectNorges forskningsråd: 315195en_US
dc.relation.projectEC/H2020/689443en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode2


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