<HashMap><database>biostudies-literature</database><scores/><additional><submitter>Kirkby J</submitter><funding>Swiss National Science Foundation</funding><funding>European Research Council</funding><funding>Natural Environment Research Council</funding><pagination>521-6</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC8384037</full_dataset_link><repository>biostudies-literature</repository><omics_type>Unknown</omics_type><volume>533(7604)</volume><pubmed_abstract>Atmospheric aerosols and their effect on clouds are thought to be important for anthropogenic radiative forcing of the climate, yet remain poorly understood. Globally, around half of cloud condensation nuclei originate from nucleation of atmospheric vapours. It is thought that sulfuric acid is essential to initiate most particle formation in the atmosphere, and that ions have a relatively minor role. Some laboratory studies, however, have reported organic particle formation without the intentional addition of sulfuric acid, although contamination could not be excluded. Here we present evidence for the formation of aerosol particles from highly oxidized biogenic vapours in the absence of sulfuric acid in a large chamber under atmospheric conditions. The highly oxygenated molecules (HOMs) ar</pubmed_abstract><journal>Nature</journal><pubmed_title>Ion-induced nucleation of pure biogenic particles.</pubmed_title><pmcid>PMC8384037</pmcid><funding_grant_id>200020</funding_grant_id><funding_grant_id>616075</funding_grant_id><funding_grant_id>135307</funding_grant_id><funding_grant_id>227463</funding_grant_id><funding_grant_id>NE/K015966/1</funding_grant_id><pubmed_authors>Gordon H</pubmed_authors><pubmed_authors>Simon M</pubmed_authors><pubmed_authors>Dias A</pubmed_authors><pubmed_authors>Molteni U</pubmed_authors><pubmed_authors>Wimmer D</pubmed_authors><pubmed_authors>Breitenlechner M</pubmed_authors><pubmed_authors>Makhmutov V</pubmed_authors><pubmed_authors>Curtius J</pubmed_authors><pubmed_authors>Carslaw KS</pubmed_authors><pubmed_authors>Heinritzi M</pubmed_authors><pubmed_authors>Chen X</pubmed_authors><pubmed_authors>Richards NA</pubmed_authors><pubmed_authors>Ortega IK</pubmed_authors><pubmed_authors>Kurten A</pubmed_authors><pubmed_authors>Worsnop DR</pubmed_authors><pubmed_authors>Sarnela N</pubmed_authors><pubmed_authors>Adamov A</pubmed_authors><pubmed_authors>Vogel AL</pubmed_authors><pubmed_authors>Onnela A</pubmed_authors><pubmed_authors>Perakyla O</pubmed_authors><pubmed_authors>Wagner R</pubmed_authors><pubmed_authors>Kangasluoma J</pubmed_authors><pubmed_authors>Stozhkov Y</pubmed_authors><pubmed_authors>Seinfeld JH</pubmed_authors><pubmed_authors>Kulmala M</pubmed_authors><pubmed_authors>Wagner PE</pubmed_authors><pubmed_authors>Almeida J</pubmed_authors><pubmed_authors>Weingartner E</pubmed_authors><pubmed_authors>Craven J</pubmed_authors><pubmed_authors>Hakala J</pubmed_authors><pubmed_authors>Winkler PM</pubmed_authors><pubmed_authors>Duplissy J</pubmed_authors><pubmed_authors>Petaja T</pubmed_authors><pubmed_authors>Brilke S</pubmed_authors><pubmed_authors>Steiner G</pubmed_authors><pubmed_authors>Frege C</pubmed_authors><pubmed_authors>Flagan RC</pubmed_authors><pubmed_authors>Donahue NM</pubmed_authors><pubmed_authors>Hoyle CR</pubmed_authors><pubmed_authors>Schobesberger S</pubmed_authors><pubmed_authors>Lehtipalo K</pubmed_authors><pubmed_authors>Ehrhart S</pubmed_authors><pubmed_authors>Kim J</pubmed_authors><pubmed_authors>Baltensperger U</pubmed_authors><pubmed_authors>Dommen J</pubmed_authors><pubmed_authors>Pringle K</pubmed_authors><pubmed_authors>Rondo L</pubmed_authors><pubmed_authors>Rap A</pubmed_authors><pubmed_authors>Williamson C</pubmed_authors><pubmed_authors>Mathot S</pubmed_authors><pubmed_authors>Virtanen A</pubmed_authors><pubmed_authors>Sipila M</pubmed_authors><pubmed_authors>Krapf M</pubmed_authors><pubmed_authors>Piel F</pubmed_authors><pubmed_authors>Amorim A</pubmed_authors><pubmed_authors>Riipinen I</pubmed_authors><pubmed_authors>Bianchi F</pubmed_authors><pubmed_authors>Sengupta K</pubmed_authors><pubmed_authors>Laaksonen A</pubmed_authors><pubmed_authors>Jokinen T</pubmed_authors><pubmed_authors>Stratmann F</pubmed_authors><pubmed_authors>Praplan AP</pubmed_authors><pubmed_authors>Wagner AC</pubmed_authors><pubmed_authors>Bernhammer AK</pubmed_authors><pubmed_authors>Franchin A</pubmed_authors><pubmed_authors>Hansel A</pubmed_authors><pubmed_authors>Rissanen MP</pubmed_authors><pubmed_authors>Scott CE</pubmed_authors><pubmed_authors>Tome A</pubmed_authors><pubmed_authors>Ye P</pubmed_authors><pubmed_authors>Zhang X</pubmed_authors><pubmed_authors>Kirkby J</pubmed_authors><pubmed_authors>Trostl J</pubmed_authors><pubmed_authors>Yan C</pubmed_authors><pubmed_authors>Junninen H</pubmed_authors><pubmed_authors>Fuchs C</pubmed_authors><pubmed_authors>Guida R</pubmed_authors><pubmed_authors>Nieminen T</pubmed_authors></additional><is_claimable>false</is_claimable><name>Ion-induced nucleation of pure biogenic particles.</name><description>Atmospheric aerosols and their effect on clouds are thought to be important for anthropogenic radiative forcing of the climate, yet remain poorly understood. Globally, around half of cloud condensation nuclei originate from nucleation of atmospheric vapours. It is thought that sulfuric acid is essential to initiate most particle formation in the atmosphere, and that ions have a relatively minor role. Some laboratory studies, however, have reported organic particle formation without the intentional addition of sulfuric acid, although contamination could not be excluded. Here we present evidence for the formation of aerosol particles from highly oxidized biogenic vapours in the absence of sulfuric acid in a large chamber under atmospheric conditions. The highly oxygenated molecules (HOMs) ar</description><dates><release>2016-01-01T00:00:00Z</release><publication>2016 May</publication><modification>2026-07-09T11:21:43.672Z</modification><creation>2026-07-09T10:46:37.233Z</creation></dates><accession>S-EPMC8384037</accession><cross_references><pubmed>27225125</pubmed><doi>10.1038/nature17953</doi></cross_references></HashMap>