EMS Annual Meeting Abstracts
Vol. 20, EMS2023-345, 2023, updated on 18 Aug 2023
https://doi.org/10.5194/ems2023-345
EMS Annual Meeting 2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.

Ice nucleation by anthropogenic aerosols downwind of industrial point sources of air pollution

Velle Toll1, Jorma Rahu1, Hannes Keernik1, Heido Trofimov1, Tanel Voormansik1, Peter Manshausen2, Emma Hung3, Daniel Michelson3, Matthew Christensen4, Piia Post1, Heikki Junninen1, Ulrike Lohmann5, Duncan Watson-Parris2, Philip Stier2, Norman Donaldson3, Trude Storelvmo6, Markku Kulmala7, Benjamin Murray8, and Nicolas Bellouin9
Velle Toll et al.
  • 1University of Tartu, Institute of Physics, Tartu, Estonia (velle.toll@ut.ee)
  • 2University of Oxford, UK
  • 3Environment and Climate Change Canada, Canada
  • 4Pacific Northwest National Laboratory, USA
  • 5ETH Zurich, Switzerland
  • 6University of Oslo, Norway
  • 7University of Helsinki, Finland
  • 8University of Leeds, UK
  • 9University of Reading, UK

Satellite observations reveal the glaciation of supercooled stratiform liquid phase clouds by anthropogenic aerosols acting as ice-nucleating particles downwind of industrial aerosol point sources. Glaciation events are observed downwind of oil refineries, coal-fired power plants, cement, metal smelting and processing, chemical plants, and other anthropogenic air pollution sources in Europe, Asia, North America and Australia. Glaciation leads to snowfall, reduced cloud cover and reduced back-scattering of solar radiation to space. The polluted areas with decreased cloud cover are plume-shaped, with a distinctive head pointing towards the pollution source, similar to aerosol-polluted cloud tracks in liquid-water clouds (Toll et al 2019 Nature https://doi.org/10.1038/s41586-019-1423-9). Moreover, heavily polluted areas derived by simulating aerosol dispersion from strong anthropogenic aerosol point sources overlap with the areas of glaciation, snowfall, and decreased cloud cover strikingly well. These lines of evidence suggest that anthropogenic aerosols are the cause of the observed glaciation events.

Glaciation-induced snowfall downwind of aerosol sources is observed using ground-based precipitation radars, and tracks of snow are also seen on the ground in satellite imagery. Thus, at least locally, anthropogenic ice nucleating particles could significantly affect precipitation amounts. At multiple aerosol sources, glaciation events are more frequent than polluted tracks in liquid-phase clouds. Thus, at least locally at some aerosol sources in the middle and high latitudes, the warming effect induced by aerosols acting as ice-nucleating particles likely exceeds the cooling effect induced by aerosols acting as cloud condensation nuclei. Further research is needed to quantify the global radiative forcing by anthropogenic ice nucleating particles.

How to cite: Toll, V., Rahu, J., Keernik, H., Trofimov, H., Voormansik, T., Manshausen, P., Hung, E., Michelson, D., Christensen, M., Post, P., Junninen, H., Lohmann, U., Watson-Parris, D., Stier, P., Donaldson, N., Storelvmo, T., Kulmala, M., Murray, B., and Bellouin, N.: Ice nucleation by anthropogenic aerosols downwind of industrial point sources of air pollution, EMS Annual Meeting 2023, Bratislava, Slovakia, 4–8 Sep 2023, EMS2023-345, https://doi.org/10.5194/ems2023-345, 2023.