Articles | Volume 21, issue 19
https://doi.org/10.5194/acp-21-15351-2021
© Author(s) 2021. 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-21-15351-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Controls on surface aerosol particle number concentrations and aerosol-limited cloud regimes over the central Greenland Ice Sheet
National Centre for Atmospheric Science, Leeds, UK
School of Earth and Environment, University of Leeds, Leeds, UK
Ian M. Brooks
School of Earth and Environment, University of Leeds, Leeds, UK
Ken S. Carslaw
School of Earth and Environment, University of Leeds, Leeds, UK
Benjamin J. Murray
School of Earth and Environment, University of Leeds, Leeds, UK
Von P. Walden
Department of Civil and Environmental Engineering, Laboratory for Atmospheric Research, Washington State University, Pullman, WA, USA
Matthew D. Shupe
Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USA
Physical Sciences Laboratory, National Oceanic and Atmospheric Administration, Boulder, CO, USA
Claire Pettersen
Space Science and Engineering Center, University of Wisconsin–Madison, Madison, WI, USA
David D. Turner
Global Systems Laboratory, National Oceanic and Atmospheric Administration, Boulder, CO, USA
Christopher J. Cox
Physical Sciences Laboratory, National Oceanic and Atmospheric Administration, Boulder, CO, USA
William D. Neff
Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO, USA
Physical Sciences Laboratory, National Oceanic and Atmospheric Administration, Boulder, CO, USA
Ralf Bennartz
Space Science and Engineering Center, University of Wisconsin–Madison, Madison, WI, USA
Earth and Environmental Sciences, Vanderbilt University, Nashville, TN, USA
Ryan R. Neely III
National Centre for Atmospheric Science, Leeds, UK
School of Earth and Environment, University of Leeds, Leeds, UK
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Cited
5 citations as recorded by crossref.
- Do Arctic mixed-phase clouds sometimes dissipate due to insufficient aerosol? Evidence from comparisons between observations and idealized simulations L. Sterzinger et al. 10.5194/acp-22-8973-2022
- Spaceborne Evidence That Ice‐Nucleating Particles Influence High‐Latitude Cloud Phase T. Carlsen & R. David 10.1029/2022GL098041
- Passive ground-based remote sensing of radiation fog H. Guy et al. 10.5194/amt-15-5095-2022
- Modification of Saharan dust size distribution during its transport over the Anatolian Plateau E. Uzunpinar et al. 10.1016/j.scitotenv.2023.164646
- Measurement report: In situ vertical profiles of below-cloud aerosol over the central Greenland Ice Sheet H. Guy et al. 10.5194/acp-24-11103-2024
5 citations as recorded by crossref.
- Do Arctic mixed-phase clouds sometimes dissipate due to insufficient aerosol? Evidence from comparisons between observations and idealized simulations L. Sterzinger et al. 10.5194/acp-22-8973-2022
- Spaceborne Evidence That Ice‐Nucleating Particles Influence High‐Latitude Cloud Phase T. Carlsen & R. David 10.1029/2022GL098041
- Passive ground-based remote sensing of radiation fog H. Guy et al. 10.5194/amt-15-5095-2022
- Modification of Saharan dust size distribution during its transport over the Anatolian Plateau E. Uzunpinar et al. 10.1016/j.scitotenv.2023.164646
- Measurement report: In situ vertical profiles of below-cloud aerosol over the central Greenland Ice Sheet H. Guy et al. 10.5194/acp-24-11103-2024
Latest update: 14 Nov 2024
Short summary
We present the first full year of surface aerosol number concentration measurements from the central Greenland Ice Sheet. Aerosol concentrations here have a distinct seasonal cycle from those at lower-altitude Arctic sites, which is driven by large-scale atmospheric circulation. Our results can be used to help understand the role aerosols might play in Greenland surface melt through the modification of cloud properties. This is crucial in a rapidly changing region where observations are sparse.
We present the first full year of surface aerosol number concentration measurements from the...
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