Articles | Volume 24, issue 22
https://doi.org/10.5194/acp-24-12595-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-24-12595-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
The annual cycle and sources of relevant aerosol precursor vapors in the central Arctic during the MOSAiC expedition
Matthew Boyer
CORRESPONDING AUTHOR
Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki, P.O. Box 64, 00014 Helsinki, Finland
Diego Aliaga
Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki, P.O. Box 64, 00014 Helsinki, Finland
Lauriane L. J. Quéléver
Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki, P.O. Box 64, 00014 Helsinki, Finland
Silvia Bucci
Department of Meteorology and Geophysics, University of Vienna, Vienna, Austria
Hélène Angot
Extreme Environments Research Laboratory, Ecole Polytechnique Fédérale de Lausanne (EPFL), 1951 Sion, Switzerland
Univ. Grenoble Alpes, CNRS, INRAE, IRD, Grenoble INP, IGE, Grenoble, France
Lubna Dada
Extreme Environments Research Laboratory, Ecole Polytechnique Fédérale de Lausanne (EPFL), 1951 Sion, Switzerland
Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland
Benjamin Heutte
Extreme Environments Research Laboratory, Ecole Polytechnique Fédérale de Lausanne (EPFL), 1951 Sion, Switzerland
Lisa Beck
Institute for Atmospheric and Environmental Sciences, Goethe University Frankfurt, 60438 Frankfurt am Main, Germany
Marina Duetsch
Department of Meteorology and Geophysics, University of Vienna, Vienna, Austria
Andreas Stohl
Department of Meteorology and Geophysics, University of Vienna, Vienna, Austria
Extreme Environments Research Laboratory, Ecole Polytechnique Fédérale de Lausanne (EPFL), 1951 Sion, Switzerland
Tiia Laurila
Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki, P.O. Box 64, 00014 Helsinki, Finland
Nina Sarnela
Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki, P.O. Box 64, 00014 Helsinki, Finland
Roseline C. Thakur
Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki, P.O. Box 64, 00014 Helsinki, Finland
Branka Miljevic
School of Earth and Atmospheric Sciences, Queensland University of Technology, Brisbane, Australia
Markku Kulmala
Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki, P.O. Box 64, 00014 Helsinki, Finland
Tuukka Petäjä
Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki, P.O. Box 64, 00014 Helsinki, Finland
Mikko Sipilä
Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki, P.O. Box 64, 00014 Helsinki, Finland
Julia Schmale
Extreme Environments Research Laboratory, Ecole Polytechnique Fédérale de Lausanne (EPFL), 1951 Sion, Switzerland
Institute for Atmospheric and Earth System Research (INAR)/Physics, Faculty of Science, University of Helsinki, P.O. Box 64, 00014 Helsinki, Finland
Climate & Atmosphere Research Centre (CARE-C), The Cyprus Institute, P.O. Box 27456, 1645 Nicosia, Cyprus
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Short summary
We analyze the seasonal cycle and sources of gases that are relevant for the formation of aerosol particles in the central Arctic. Since theses gases can form new particles, they can influence Arctic climate. We show that the sources of these gases are associated with changes in the Arctic environment during the year, especially with respect to sea ice. Therefore, the concentration of these gases will likely change in the future as the Arctic continues to warm.
We analyze the seasonal cycle and sources of gases that are relevant for the formation of...
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