Ozone concentration measured during the Arctic Ocean 2018 expedition
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. Ozone is a trace gas that can be formed directly in the troposphere (the most important formation pathway is the photochemical reactio...
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ftinfoscience:oai:infoscience.epfl.ch:283447 2023-05-15T14:51:29+02:00 Ozone concentration measured during the Arctic Ocean 2018 expedition Baccarini, Andrea Schmale, Julia Dommen, Josef 2021-02-22T19:01:03Z https://doi.org/10.17043/ao2018-aerosol-ozone http://infoscience.epfl.ch/record/283447 unknown doi:10.17043/ao2018-aerosol-ozone http://infoscience.epfl.ch/record/283447 http://infoscience.epfl.ch/record/283447 Text 2021 ftinfoscience https://doi.org/10.17043/ao2018-aerosol-ozone 2023-02-13T23:03:32Z 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. Ozone 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. Measurements were performed on the 4th deck of icebreaker Oden during August and September 2018 along the track of the Arctic Ocean 2018 expedition. Text Arctic Arctic Ocean oden EPFL Infoscience (Ecole Polytechnique Fédérale Lausanne) Arctic Arctic Ocean |
institution |
Open Polar |
collection |
EPFL Infoscience (Ecole Polytechnique Fédérale Lausanne) |
op_collection_id |
ftinfoscience |
language |
unknown |
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. Ozone 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. Measurements were performed on the 4th deck of icebreaker Oden during August and September 2018 along the track of the Arctic Ocean 2018 expedition. |
format |
Text |
author |
Baccarini, Andrea Schmale, Julia Dommen, Josef |
spellingShingle |
Baccarini, Andrea Schmale, Julia Dommen, Josef Ozone concentration measured during the Arctic Ocean 2018 expedition |
author_facet |
Baccarini, Andrea Schmale, Julia Dommen, Josef |
author_sort |
Baccarini, Andrea |
title |
Ozone concentration measured during the Arctic Ocean 2018 expedition |
title_short |
Ozone concentration measured during the Arctic Ocean 2018 expedition |
title_full |
Ozone concentration measured during the Arctic Ocean 2018 expedition |
title_fullStr |
Ozone concentration measured during the Arctic Ocean 2018 expedition |
title_full_unstemmed |
Ozone concentration measured during the Arctic Ocean 2018 expedition |
title_sort |
ozone concentration measured during the arctic ocean 2018 expedition |
publishDate |
2021 |
url |
https://doi.org/10.17043/ao2018-aerosol-ozone http://infoscience.epfl.ch/record/283447 |
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/283447 |
op_relation |
doi:10.17043/ao2018-aerosol-ozone http://infoscience.epfl.ch/record/283447 |
op_doi |
https://doi.org/10.17043/ao2018-aerosol-ozone |
_version_ |
1766322615174037504 |