EGU24-20594, updated on 11 Mar 2024
https://doi.org/10.5194/egusphere-egu24-20594
EGU General Assembly 2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

Sea ice, snow caps, and freshwater lenses: The hurdles local Arctic aerosols must overcome to become airborne

Jessie Creamean1 and the MOSAiC and ARTofMELT field teams*
Jessie Creamean and the MOSAiC and ARTofMELT field teams
  • 1Colorado State University, Atmospheric Science, Fort Collins, United States of America
  • *A full list of authors appears at the end of the abstract

Aerosol particles and clouds play a critical role in regulating radiation reaching the Arctic, which is warming faster than anywhere else globally. However, the magnitude of their effects is not adequately quantified, especially in the Arctic Ocean over sea ice. Specifically, particles generated from open leads, melt ponds, and the snow-covered sea ice surfaces remain poorly understood, yet could have significant impacts on cloud condensation nuclei (CCN) and ice nucleating particle (INP) concentrations, and thus, central Arctic cloud formation. While marine biological processes have been demonstrated to be potentially key primary aerosol sources in the Arctic summer, exact sources and emission processes of these particles remain highly uncertain. 

For this presentation, we provide an overview of aerosol observations from two recent Arctic field campaigns: the 2019–2020 Multidisciplinary drifting Observatory for Study of Arctic Climate (MOSAiC) and the 2023 Atmospheric rivers and the onset of Arctic melt (ARTofMELT) expeditions. We highlight preliminary findings focused on aerosols that have the potential to impact cloud phase and lifetime over the Arctic Ocean, specifically those from local sources in the early spring and summer melt periods. The evolution of open water within the pack ice in late spring and the Arctic melt season coincides with an increase in aerosol particle concentration, which may be attributed to biological activity within seawater and sea ice. However, the emission of aerosol particles is contingent on features like open leads and melt ponds, and whether they are covered by snow, freshwater melt layers, or ice lids. This integrative study involves the use of detailed aerosol, meteorological, oceanographic, and sea ice observations from MOSAiC and ARTofMELT. Overall, this work will enable us to assess local aerosol processes associated with cloud formation to better understand the Arctic system through a holistic approach.

MOSAiC and ARTofMELT field teams:

Camille Mavis, Kevin Barry, Ivo Beck, Nora Bergner, Benjamin Heutte, Jessica Mirrielees, Jennie Spicker Schmidt, Nicolas Fauré, Gabriel Freitas, Julia Asplund, Fredrik Mattsson, Lovisa Nilsson, Lea Haberstock, Luisa Ickes, Stella Papadopoulou, Thomas Hill, Paul DeMott, Julia Schmale, Kerri Pratt, Tina Šantl-Temkiv, Erik S. Thomson, Paul Zieger

How to cite: Creamean, J. and the MOSAiC and ARTofMELT field teams: Sea ice, snow caps, and freshwater lenses: The hurdles local Arctic aerosols must overcome to become airborne, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-20594, https://doi.org/10.5194/egusphere-egu24-20594, 2024.