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dc.contributor.authorPetrenko, Mariya
dc.contributor.authorKahn, Ralph
dc.contributor.authorChin, Mian
dc.contributor.authorBauer, Susanne
dc.contributor.authorBergman, Tommi
dc.contributor.authorBian, Huisheng
dc.contributor.authorCurci, Gabriele
dc.contributor.authorJohnson, Ben
dc.contributor.authorKaiser, Johannes
dc.contributor.authorKipling, Zak
dc.contributor.authorKokkola, Harri
dc.contributor.authorLiu, Xiaohong
dc.contributor.authorMezuman, Keren
dc.contributor.authorMielonen, Tero
dc.contributor.authorMyhre, Gunnar
dc.contributor.authorPan, Xiaohua
dc.contributor.authorProtonotariou, Anna
dc.contributor.authorRemy, Samuel
dc.contributor.authorSkeie, Ragnhild Bieltvedt
dc.contributor.authorStier, Philip
dc.contributor.authorToshihiko, Takemura
dc.contributor.authorTsigaridis, Kostas
dc.contributor.authorWang, Hailong
dc.contributor.authorWatson-Parris, Duncan
dc.contributor.authorZhang, Kai
dc.date.accessioned2025-02-10T13:47:40Z
dc.date.available2025-02-10T13:47:40Z
dc.date.created2025-02-05T15:15:03Z
dc.date.issued2025
dc.identifier.citationAtmospheric Chemistry and Physics (ACP). 2025, 25 (3), 1545-1567.en_US
dc.identifier.issn1680-7316
dc.identifier.urihttps://hdl.handle.net/11250/3177170
dc.description.abstractWe assessed the biomass burning (BB) smoke aerosol optical depth (AOD) simulations of 11 global models that participated in the AeroCom phase III BB emission experiment. By comparing multi-model simulations and satellite observations in the vicinity of fires over 13 regions globally, we (1) assess model-simulated BB AOD performance as an indication of smoke source–strength, (2) identify regions where the common emission dataset used by the models might underestimate or overestimate smoke sources, and (3) assess model diversity and identify underlying causes as much as possible. Using satellite-derived AOD snapshots to constrain source strength works best where BB smoke from active sources dominates background non-BB aerosol, such as in boreal forest regions and over South America and southern hemispheric Africa. The comparison is inconclusive where the total AOD is low, as in many agricultural burning areas, and where the background is high, such as parts of India and China. Many inter-model BB AOD differences can be traced to differences in values for the mass ratio of organic aerosol to organic carbon, the BB aerosol mass extinction efficiency, and the aerosol loss rate from each model. The results point to a need for increased numbers of available BB cases for study in some regions and especially to a need for more extensive regional-to-global-scale measurements of aerosol loss rates and of detailed particle microphysical and optical properties; this would both better constrain models and help distinguish BB from other aerosol types in satellite retrievals. More generally, there is the need for additional efforts at constraining aerosol source strength and other model attributes with multi-platform observations.en_US
dc.description.abstractBiomass burning emission analysis based on MODISen_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.titleBiomass burning emission analysis based on MODISen_US
dc.title.alternativeBiomass burning emission analysis based on MODISen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.source.pagenumber1545-1567en_US
dc.source.volume25en_US
dc.source.journalAtmospheric Chemistry and Physics (ACP)en_US
dc.source.issue3en_US
dc.identifier.doi10.5194/acp-25-1545-2025
dc.identifier.cristin2356518
dc.relation.projectNILU: 124007en_US
cristin.ispublishedtrue
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