Articles | Volume 19, issue 22
https://doi.org/10.5194/acp-19-14339-2019
© Author(s) 2019. 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-19-14339-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
New particle formation and its effect on cloud condensation nuclei abundance in the summer Arctic: a case study in the Fram Strait and Barents Sea
Simonas Kecorius
CORRESPONDING AUTHOR
Leibniz Institute for Tropospheric Research (TROPOS), 04318 Leipzig, Germany
Teresa Vogl
Leibniz Institute for Tropospheric Research (TROPOS), 04318 Leipzig, Germany
Institute for Meteorology, University of Leipzig, 04103 Leipzig,
Germany
Pauli Paasonen
Department of Physics, University of Helsinki, P.O. Box 64, 00014
Helsinki, Finland
Janne Lampilahti
Department of Physics, University of Helsinki, P.O. Box 64, 00014
Helsinki, Finland
Daniel Rothenberg
ClimaCell, Inc., Boston, 02210 Massachusetts, USA
Heike Wex
Leibniz Institute for Tropospheric Research (TROPOS), 04318 Leipzig, Germany
Sebastian Zeppenfeld
Leibniz Institute for Tropospheric Research (TROPOS), 04318 Leipzig, Germany
Manuela van Pinxteren
Leibniz Institute for Tropospheric Research (TROPOS), 04318 Leipzig, Germany
Markus Hartmann
Leibniz Institute for Tropospheric Research (TROPOS), 04318 Leipzig, Germany
Silvia Henning
Leibniz Institute for Tropospheric Research (TROPOS), 04318 Leipzig, Germany
Xianda Gong
Leibniz Institute for Tropospheric Research (TROPOS), 04318 Leipzig, Germany
Andre Welti
Leibniz Institute for Tropospheric Research (TROPOS), 04318 Leipzig, Germany
Markku Kulmala
Department of Physics, University of Helsinki, P.O. Box 64, 00014
Helsinki, Finland
Frank Stratmann
Leibniz Institute for Tropospheric Research (TROPOS), 04318 Leipzig, Germany
Hartmut Herrmann
Leibniz Institute for Tropospheric Research (TROPOS), 04318 Leipzig, Germany
Alfred Wiedensohler
Leibniz Institute for Tropospheric Research (TROPOS), 04318 Leipzig, Germany
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34 citations as recorded by crossref.
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- The annual cycle and sources of relevant aerosol precursor vapors in the central Arctic during the MOSAiC expedition M. Boyer et al. 10.5194/acp-24-12595-2024
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- Seasonal observation and source apportionment of carbonaceous aerosol from forested rural site (Lithuania) A. Masalaite et al. 10.1016/j.atmosenv.2021.118934
- Application of the shipborne remote sensing supersite OCEANET for profiling of Arctic aerosols and clouds during <i>Polarstern</i> cruise PS106 H. Griesche et al. 10.5194/amt-13-5335-2020
- Use of aircraft in ocean alkalinity enhancement E. Gentile et al. 10.1016/j.scitotenv.2022.153484
- Natural Marine Precursors Boost Continental New Particle Formation and Production of Cloud Condensation Nuclei R. de Jonge et al. 10.1021/acs.est.4c01891
- Atmospheric VOC measurements at a High Arctic site: characteristics and source apportionment J. Pernov et al. 10.5194/acp-21-2895-2021
- Tethered balloon measurements reveal enhanced aerosol occurrence aloft interacting with Arctic low-level clouds C. Pilz et al. 10.1525/elementa.2023.00120
- Dimethyl Sulfide‐Induced Increase in Cloud Condensation Nuclei in the Arctic Atmosphere K. Park et al. 10.1029/2021GB006969
- Rapid growth of Aitken-mode particles during Arctic summer by fog chemical processing and its implication S. Kecorius et al. 10.1093/pnasnexus/pgad124
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- Revealing the chemical characteristics of Arctic low-level cloud residuals – in situ observations from a mountain site Y. Gramlich et al. 10.5194/acp-23-6813-2023
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- Valine involved sulfuric acid-dimethylamine ternary homogeneous nucleation and its atmospheric implications Y. Liu et al. 10.1016/j.atmosenv.2021.118373
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Latest update: 14 Dec 2024
Short summary
Arctic sea-ice retreat, atmospheric new particle formation (NPF), and aerosol–cloud interaction may all be linked via a positive feedback mechanism. Understanding the sources of cloud condensation nuclei (CCN) is an important piece in the Arctic amplification puzzle. We show that Arctic newly formed particles do not have to grow beyond the Aitken mode to act as CCN. This is important, because NPF occurrence in the Arctic is expected to increase, making it a significant contributor to CCN budget.
Arctic sea-ice retreat, atmospheric new particle formation (NPF), and aerosol–cloud interaction...
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