Concentration of particles larger than 2.5 nm collected during the Arctic Ocean 2018 expedition
The concentration of particles larger than 2.5 nm was measured with an ultrafine condensation particle counter (UCPC). The concentration was corrected for diffusional losses in the inlet based on the neutral cluster and air ion spectrometer (NAIS) size distribution. The concentration and temporal dy...
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ftinfoscience:oai:infoscience.epfl.ch:283438 2023-05-15T15:01:09+02:00 Concentration of particles larger than 2.5 nm collected during the Arctic Ocean 2018 expedition Baccarini, Andrea Schmale, Julia Dommen, Josef 2021-02-22T18:51:09Z https://doi.org/10.17043/ao2018-aerosol-ucpc http://infoscience.epfl.ch/record/283438 unknown doi:10.17043/ao2018-aerosol-ucpc http://infoscience.epfl.ch/record/283438 http://infoscience.epfl.ch/record/283438 Text 2021 ftinfoscience https://doi.org/10.17043/ao2018-aerosol-ucpc 2023-02-13T23:03:32Z The concentration of particles larger than 2.5 nm was measured with an ultrafine condensation particle counter (UCPC). The concentration was corrected for diffusional losses in the inlet based on the neutral cluster and air ion spectrometer (NAIS) size distribution. The concentration and temporal dynamics of small particles is fundamental to characterize the first step of new particle formation (NPF) and growth. Newly formed particles can grow to larger sizes where they act as cloud condensation nuclei, directly affecting the Earth radiative budget and cloud properties. Measurements 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 particle per cubic centimeter in 60 seconds average. Text Arctic Arctic Ocean oden EPFL Infoscience (Ecole Polytechnique Fédérale Lausanne) Arctic Arctic Ocean |
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Open Polar |
collection |
EPFL Infoscience (Ecole Polytechnique Fédérale Lausanne) |
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ftinfoscience |
language |
unknown |
description |
The concentration of particles larger than 2.5 nm was measured with an ultrafine condensation particle counter (UCPC). The concentration was corrected for diffusional losses in the inlet based on the neutral cluster and air ion spectrometer (NAIS) size distribution. The concentration and temporal dynamics of small particles is fundamental to characterize the first step of new particle formation (NPF) and growth. Newly formed particles can grow to larger sizes where they act as cloud condensation nuclei, directly affecting the Earth radiative budget and cloud properties. Measurements 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 particle per cubic centimeter in 60 seconds average. |
format |
Text |
author |
Baccarini, Andrea Schmale, Julia Dommen, Josef |
spellingShingle |
Baccarini, Andrea Schmale, Julia Dommen, Josef Concentration of particles larger than 2.5 nm collected during the Arctic Ocean 2018 expedition |
author_facet |
Baccarini, Andrea Schmale, Julia Dommen, Josef |
author_sort |
Baccarini, Andrea |
title |
Concentration of particles larger than 2.5 nm collected during the Arctic Ocean 2018 expedition |
title_short |
Concentration of particles larger than 2.5 nm collected during the Arctic Ocean 2018 expedition |
title_full |
Concentration of particles larger than 2.5 nm collected during the Arctic Ocean 2018 expedition |
title_fullStr |
Concentration of particles larger than 2.5 nm collected during the Arctic Ocean 2018 expedition |
title_full_unstemmed |
Concentration of particles larger than 2.5 nm collected during the Arctic Ocean 2018 expedition |
title_sort |
concentration of particles larger than 2.5 nm collected during the arctic ocean 2018 expedition |
publishDate |
2021 |
url |
https://doi.org/10.17043/ao2018-aerosol-ucpc http://infoscience.epfl.ch/record/283438 |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
Arctic Arctic Ocean oden |
genre_facet |
Arctic Arctic Ocean oden |
op_source |
http://infoscience.epfl.ch/record/283438 |
op_relation |
doi:10.17043/ao2018-aerosol-ucpc http://infoscience.epfl.ch/record/283438 |
op_doi |
https://doi.org/10.17043/ao2018-aerosol-ucpc |
_version_ |
1766333194557194240 |