{"database":"biostudies-literature","file_versions":[],"scores":null,"additional":{"submitter":["Stolzenburg D"],"funding":["Austrian Science Fund FWF","Swiss National Science Foundation","European Research Council"],"pagination":["9122-9127"],"full_dataset_link":["https://www.ebi.ac.uk/biostudies/studies/S-EPMC6140529"],"repository":["biostudies-literature"],"omics_type":["Unknown"],"volume":["115(37)"],"pubmed_abstract":["Nucleation and growth of aerosol particles from atmospheric vapors constitutes a major source of global cloud condensation nuclei (CCN). The fraction of newly formed particles that reaches CCN sizes is highly sensitive to particle growth rates, especially for particle sizes <10 nm, where coagulation losses to larger aerosol particles are greatest. Recent results show that some oxidation products from biogenic volatile organic compounds are major contributors to particle formation and initial growth. However, whether oxidized organics contribute to particle growth over the broad span of tropospheric temperatures remains an open question, and quantitative mass balance for organic growth has yet to be demonstrated at any temperature. Here, in experiments performed under atmospheric conditions"],"journal":["Proceedings of the National Academy of Sciences of the United States of America"],"pubmed_title":["Rapid growth of organic aerosol nanoparticles over a wide tropospheric temperature range."],"pmcid":["PMC6140529"],"funding_grant_id":["692891","638703","200020","616075","307331","656994","J 3951","159851","742206"],"pubmed_authors":["Baccarini A","Lawler M","Simon M","Gordon H","Dias A","Molteni U","Draper DC","Wimmer D","Dada L","Quelever LLJ","Breitenlechner M","El Haddad I","Stolzenburg D","Wang M","Leiminger M","Ahonen LR","Bauer PS","Curtius J","Helm J","Heinritzi M","Kurten A","Worsnop DR","Sarnela N","Buenrostro Mazon S","Bergen A","Schallhart S","Kontkanen J","Vogel AL","Onnela A","Chen D","Tauber C","Wagner R","He X","Kulmala M","Fischer L","Kim C","Winkler PM","Duplissy J","Petaja T","Brilke S","Frege C","Flagan RC","Donahue NM","Hoyle CR","Finkenzeller H","Lehtipalo K","Schervish M","Baltensperger U","Dommen J","Mentler B","Mathot S","Passananti M","Nie W","Zha Q","Amorim A","Bianchi F","Smith JN","Wagner AC","Hansel A","Lampilahti J","Hofbauer V","Rissanen MP","Garmash O","Nowak JB","Tome A","Xiao M","Ye P","Mai H","Weitz L","Baumgartner B","Kirkby J","Yan C","Fuchs C","Ojdanic A","Nieminen T"],"additional_accession":[]},"is_claimable":false,"name":"Rapid growth of organic aerosol nanoparticles over a wide tropospheric temperature range.","description":"Nucleation and growth of aerosol particles from atmospheric vapors constitutes a major source of global cloud condensation nuclei (CCN). The fraction of newly formed particles that reaches CCN sizes is highly sensitive to particle growth rates, especially for particle sizes <10 nm, where coagulation losses to larger aerosol particles are greatest. Recent results show that some oxidation products from biogenic volatile organic compounds are major contributors to particle formation and initial growth. However, whether oxidized organics contribute to particle growth over the broad span of tropospheric temperatures remains an open question, and quantitative mass balance for organic growth has yet to be demonstrated at any temperature. Here, in experiments performed under atmospheric conditions","dates":{"release":"2018-01-01T00:00:00Z","publication":"2018 Sep","modification":"2025-04-04T09:26:47.111Z","creation":"2019-03-26T23:56:26Z"},"accession":"S-EPMC6140529","cross_references":{"pubmed":["30154167"],"doi":["10.1073/pnas.1807604115"]}}