Articles | Volume 24, issue 7
https://doi.org/10.5194/acp-24-4537-2024
© Author(s) 2024. 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-24-4537-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Soot aerosols from commercial aviation engines are poor ice-nucleating particles at cirrus cloud temperatures
Institute for Atmospheric and Climate Science, ETH Zürich, Zürich, Switzerland
Lukas Durdina
Centre for Aviation, ZHAW School of Engineering, Winterthur, Switzerland
Peter A. Alpert
Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen PSI, Switzerland
Fabian Mahrt
Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen PSI, Switzerland
Christopher H. Dreimol
Wood Materials Science, Institute for Building Materials, ETH Zürich, Zürich, Switzerland
Cellulose & Wood Materials Laboratory, Empa, Dübendorf, Switzerland
Jacinta Edebeli
Centre for Aviation, ZHAW School of Engineering, Winterthur, Switzerland
Curdin Spirig
Centre for Aviation, ZHAW School of Engineering, Winterthur, Switzerland
Zachary C. J. Decker
Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen PSI, Switzerland
Julien Anet
Centre for Aviation, ZHAW School of Engineering, Winterthur, Switzerland
Institute for Atmospheric and Climate Science, ETH Zürich, Zürich, Switzerland
Data sets
Soot aerosol from commercial aviation engines are poor ice nucleating particles at cirrus cloud temperatures Baptiste Testa, Lukas Durdina, Peter A. Alpert, Fabian Mahrt, Christopher H. Dreimol, Jacinta Edebeli, Curdin Spirig, Zachary C.J. Decker, Julien Anet, and Zamin A. Kanji https://doi.org/10.3929/ethz-b-000634341
Short summary
Laboratory experiments on the ice nucleation of real commercial aviation soot particles are investigated for their cirrus cloud formation potential. Our results show that aircraft-emitted soot in the upper troposphere will be poor ice-nucleating particles. Measuring the soot particle morphology and modifying their mixing state allow us to elucidate why these particles are ineffective at forming ice, in contrast to previously used soot surrogates.
Laboratory experiments on the ice nucleation of real commercial aviation soot particles are...
Altmetrics
Final-revised paper
Preprint