Articles | Volume 18, issue 7
https://doi.org/10.5194/acp-18-4477-2018
© Author(s) 2018. 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-18-4477-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
04 Apr 2018
Research article |
| 04 Apr 2018
| 04 Apr 2018
Measurements of aerosol and CCN properties in the Mackenzie River delta (Canadian Arctic) during spring–summer transition in May 2014
Paul Herenz
Leibniz Institute for Tropospheric Research, Leipzig, Germany
Heike Wex
Leibniz Institute for Tropospheric Research, Leipzig, Germany
Silvia Henning
Leibniz Institute for Tropospheric Research, Leipzig, Germany
Thomas Bjerring Kristensen
Leibniz Institute for Tropospheric Research, Leipzig, Germany
now at: Division of Nuclear Physics, Lund University, Box 118, Lund 22100, Sweden
Florian Rubach
Particle Chemistry Department, Max Planck Institute for Chemistry, Mainz, Germany
Anja Roth
Particle Chemistry Department, Max Planck Institute for Chemistry, Mainz, Germany
Stephan Borrmann
Particle Chemistry Department, Max Planck Institute for Chemistry, Mainz, Germany
Heiko Bozem
Institute for Atmospheric Physics, Johannes Gutenberg University, Mainz, Germany
Hannes Schulz
Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany
Frank Stratmann
CORRESPONDING AUTHOR
Leibniz Institute for Tropospheric Research, Leipzig, Germany
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20 citations as recorded by crossref.
- Aerosol and dynamical contributions to cloud droplet formation in Arctic low-level clouds G. Motos et al. 10.5194/acp-23-13941-2023
- Nonturbulent Liquid‐Bearing Polar Clouds: Observed Frequency of Occurrence and Simulated Sensitivity to Gravity Waves I. Silber et al. 10.1029/2020GL087099
- Characterizing the hygroscopicity of growing particles in the Canadian Arctic summer R. Chang et al. 10.5194/acp-22-8059-2022
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- Relationship between cloud condensation nuclei (CCN) concentration and aerosol optical depth in the Arctic region S. Ahn et al. 10.1016/j.atmosenv.2021.118748
- Measurement report: The chemical composition of and temporal variability in aerosol particles at Tuktoyaktuk, Canada, during the Year of Polar Prediction Second Special Observing Period J. MacInnis et al. 10.5194/acp-21-14199-2021
- Annual variability of ice-nucleating particle concentrations at different Arctic locations H. Wex et al. 10.5194/acp-19-5293-2019
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- Measurement report: High Arctic aerosol hygroscopicity at sub- and supersaturated conditions during spring and summer A. Massling et al. 10.5194/acp-23-4931-2023
- Efficacy of a portable, moderate-resolution, fast-scanning differential mobility analyzer for ambient aerosol size distribution measurements S. Amanatidis et al. 10.5194/amt-14-4507-2021
- Hygroscopicity and CCN Activity of Water‐Soluble Extracts From the Arctic Aerosols in Winter to Early Summer K. Kawana et al. 10.1029/2021JD035979
- Aerosol size distribution properties associated with cold-air outbreaks in the Norwegian Arctic A. Williams et al. 10.5194/acp-24-11791-2024
- CCN measurements at the Princess Elisabeth Antarctica research station during three austral summers P. Herenz et al. 10.5194/acp-19-275-2019
- Characterization of aerosol properties at Cyprus, focusing on cloud condensation nuclei and ice-nucleating particles X. Gong et al. 10.5194/acp-19-10883-2019
- Characterization of aerosol particles at Cabo Verde close to sea level and at the cloud level – Part 1: Particle number size distribution, cloud condensation nuclei and their origins X. Gong et al. 10.5194/acp-20-1431-2020
- Maximum Supersaturation in the Marine Boundary Layer Clouds Over the North Atlantic X. Gong et al. 10.1029/2022AV000855
- Comparison of Antarctic and Arctic Single‐Layer Stratiform Mixed‐Phase Cloud Properties Using Ground‐Based Remote Sensing Measurements D. Zhang et al. 10.1029/2019JD030673
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Latest update: 20 Nov 2024
Short summary
The Arctic climate is changing much faster than other regions on Earth. Hence, it is necessary to investigate the processes that are liable for this phenomena and to document the current situation in the Arctic. Therefore, we measured the number and also the size of aerosol particles. It turned out that we captured the transition from the Arctic spring to the Arctic summer and that the according air masses show differences in particle properties. Also, the particles have a low water receptivity.
The Arctic climate is changing much faster than other regions on Earth. Hence, it is necessary...
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