[{"@context":"http:\/\/schema.org\/","@type":"Dataset","identifier":"https:\/\/doi.org\/10.17043\/oden-ao-2018-aerosol-smps-1","@id":"https:\/\/doi.org\/10.17043\/oden-ao-2018-aerosol-smps-1","name":"Size distribution of interstitial and total particles between 18 and 660 nm collected during the Arctic Ocean 2018 expedition","description":"The aerosol size distribution was measured with a custom made scanning mobility particle sizer (SMPS), range 18\u2060\u200a\u2013\u200a\u2060660 nm.\r\n\r\nAerosols are important for a variety of reasons, one of the most prominent is that a sub-set of the aerosol population can act as cloud condensation nuclei (CCN) influencing cloud formation and the Earth radiative budget. The measurements reported here can be used to investigate aerosol sources and processes. Moreover, an interstitial inlet was used to characterize the interstitial aerosol population during fog events.\r\n\r\nMeasurements were performed on the 4th deck of icebreaker Oden during August and September 2018 along the track of the expedition. The concentration is reported as dN\/dlog(Dp) per cubic centimeter with a 3 minutes time resolution.","url":"http:\/\/bolin.su.se\/data\/oden-ao-2018-aerosol-smps-1","keywords":["Atmosphere","Aerosols","Aerosol physical properties","Aerosols","AO2018","Arctic Ocean","Icebreaker Oden","Atmosphere","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","Scanning mobility particle sizer","SMPS","Aerosol size distribution","Earth science > Atmosphere"],"creator":{"@type":"Person","name":"Andrea Baccarini, Julia Schmale"},"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\nWang SC, Flagan RC (1989) Scanning Electrical Mobility Spectrometer. J. Aerosol Sci. 20:1485\u2060\u200a\u2013\u200a\u20601488. doi:10.1080\/02786829008959441","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-smps.csv"},"size":25105997,"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\nWang SC, Flagan RC (1989) Scanning Electrical Mobility Spectrometer. J. Aerosol Sci. 20:1485\u2060\u200a\u2013\u200a\u20601488. doi:10.1080\/02786829008959441","temporalCoverage":"2018-08-16\/2018-08-16"}]