{"refrec":{"BRefID":324985,"RR":"<b>Schill, G.P.; Froyd, K.D.; Bian, H.; Kupc, A.; Williamson, C.; Brock, C.A.; Ray, E.; Hornbrook, R.S.; Hills, A.J.; Apel, E.C.; Chin, M.; Colarco, P.R.; Murphy, D.M.</b> (2020). Widespread biomass burning smoke throughout the remote troposphere. <i>Nature Geoscience 13(6)</i>: 422-427. <a href=\"https://dx.doi.org/10.1038/s41561-020-0586-1\" target=\"_blank\">https://dx.doi.org/10.1038/s41561-020-0586-1</a>","BEntID":318462,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nature Geoscience 13(6)</i>: 422-427. <a href=\"https://dx.doi.org/10.1038/s41561-020-0586-1\" target=\"_blank\">https://dx.doi.org/10.1038/s41561-020-0586-1</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Schill, G.P.; Froyd, K.D.; Bian, H.; Kupc, A.; Williamson, C.; Brock, C.A.; Ray, E.; Hornbrook, R.S.; Hills, A.J.; Apel, E.C.; Chin, M.; Colarco, P.R.; Murphy, D.M.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Schill, G.P. <i>et al.</i>","Englishabstract":"Biomass burning emits ~34–41 Tg yr<sup>−1</sup> of smoke aerosol to the atmosphere. Biomass burning aerosol directly influences the Earth’s climate by attenuation of solar and terrestrial radiation; however, its abundance and distribution on a global scale are poorly constrained, particularly after plumes dilute into the background remote troposphere and are subject to removal by clouds and precipitation. Here we report global-scale, airborne measurements of biomass burning aerosol in the remote troposphere. Measurements were taken during four series of seasonal flights over the Pacific and Atlantic Ocean basins, each with near pole-to-pole latitude coverage. We find that biomass burning particles in the remote troposphere are dilute but ubiquitous, accounting for one-quarter of the accumulation-mode aerosol number and one-fifth of the aerosol mass. Comparing our observations with a high-resolution global aerosol model, we find that the model overestimates biomass burning aerosol mass in the remote troposphere with a mean bias of &gt;400%, largely due to insufficient wet removal by in-cloud precipitation. After updating the model’s aerosol removal scheme we find that, on a global scale, dilute smoke contributes as much as denser plumes to biomass burning’s scattering and absorption effects on the Earth’s radiation field.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Widespread biomass burning smoke throughout the remote troposphere","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2020,"MonPub":null,"DateUpdate":"2020-06-10","DateCreate":"2020-06-10","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000539293600007","VABBcode":null,"OpenAcc":0,"DOI":"10.1038/s41561-020-0586-1"},"refs":null,"anarec":{"AnaID":324985,"PubliDate":2020,"Pagination":"422-427","XtraPublOfAnaID":null,"ISBN":null,"Volume":"13","Issue":"6","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":123796,"SerRR":"Nature Geoscience. 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