[{"@context":"http:\/\/schema.org\/","@type":"Dataset","identifier":"https:\/\/doi.org\/10.17043\/oden-ao-2018-aerosol-ozone-1","@id":"https:\/\/doi.org\/10.17043\/oden-ao-2018-aerosol-ozone-1","name":"Ozone concentration measured during the Arctic Ocean 2018 expedition","description":"Ozone was measured with a 2B Technology ozone monitor (model 205). The concentration is reported as a mixing ratio in parts per billion [ppb], at 60 seconds average.\r\n\r\nOzone is a trace gas that can be formed directly in the troposphere (the most important formation pathway is the photochemical reaction of volatile organic compounds with NO,,x,,) or entrained from the stratosphere where it is formed directly from the reaction of molecular oxygen with UV light. Ozone is an important oxidant in the atmosphere and participate in several chemical reactions.\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-ozone-1","keywords":["Atmosphere","Trace gases","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","Ozone","Trace gas","Tropospheric chemistry","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","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-ozone.csv"},"size":2731370,"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","temporalCoverage":"2018-08-01\/2018-08-01"}]