[{"@context":"http:\/\/schema.org\/","@type":"Dataset","identifier":"https:\/\/doi.org\/10.17043\/oden-ao-2018-aerosol-condensation-sink-1","@id":"https:\/\/doi.org\/10.17043\/oden-ao-2018-aerosol-condensation-sink-1","name":"Sulfuric acid condensation sink calculated for the Arctic Ocean 2018 expedition","description":"The condensation sink is a measure of the sulfuric acid lifetime against condensation on preexisting aerosol particles. Dimensionally it is the inverse of a time (reported in per second) and it is calculated starting from the aerosol size distribution.\r\n\r\nA large condensation sink means that sulfuric acid and other gaseous species with a similarly low volatility (e.g., iodic and methanesufonic acid) will rapidly condense and their atmospheric concentration will decrease.\r\n\r\nMeasurements were performed on the 4th deck of icebreaker Oden during August and September 2018 along the track of the Arctic Ocean 2018 expedition.","url":"http:\/\/bolin.su.se\/data\/oden-ao-2018-aerosol-condensation-sink-1","keywords":["Atmosphere","Gas phase","Atmospheric gas phase data","AO2018","Arctic Ocean","Icebreaker Oden","Arctic Ocean 2018","Atmospheric Science","Atmospheric Chemistry","Atmospheric Physics","Clouds Aerosol Science","Microbiology-Ocean-Cloud-Coupling in the High Arctic","MOCCHA","High Arctic","North Pole","Aerosol-Cloud-Interaction 2018","Condensation sink","New particle formation","Earth science > Atmosphere"],"creator":{"@type":"Person","name":"Andrea Baccarini, Julia Schmale, Josef Dommen"},"citation":"Baccarini A, Karlsson L, Dommen J, Duplessis P, V\u00fcllers J, Brooks IM, Saiz-Lopez A, Salter M, Tjernstr\u00f6m M, Baltensperger U, Zieger P, Schmale J (2020) Frequent new particle formation over the high Arctic pack ice by enhanced iodine emissions. Nature Communications 11:4924. doi:10.1038\/s41467-020-18551-0\r\n\r\nDal Maso M et al. (2002) Condensation and coagulation sinks and formation of nucleation mode particles in coastal and boreal forest boundary layers. J. Geophys. Res. Atmos. 107. doi:10.1029\/2001JD001053","license":"https:\/\/creativecommons.org\/licenses\/by\/4.0\/","isAccessibleForFree":true,"includedInDataCatalog":{"@type":"DataCatalog","name":"Bolin Centre for Climate Research, Stockholm University","identifier":"https:\/\/bolin.su.se\/data\/","url":"https:\/\/bolin.su.se\/data\/"},"distribution":{"@type":"DataDownload","encodingFormat":"text\/plain","contentUrl":"https:\/\/bolin.su.se\/data\/uploads\/ao2018-aerosol-condensation-sink.csv"},"size":222082,"isBasedOn":"Baccarini A, Karlsson L, Dommen J, Duplessis P, V\u00fcllers J, Brooks IM, Saiz-Lopez A, Salter M, Tjernstr\u00f6m M, Baltensperger U, Zieger P, Schmale J (2020) Frequent new particle formation over the high Arctic pack ice by enhanced iodine emissions. Nature Communications 11:4924. doi:10.1038\/s41467-020-18551-0\r\n\r\nDal Maso M et al. (2002) Condensation and coagulation sinks and formation of nucleation mode particles in coastal and boreal forest boundary layers. J. Geophys. Res. Atmos. 107. doi:10.1029\/2001JD001053","temporalCoverage":"2018-08-02\/2018-08-02"}]