Articles | Volume 22, issue 2
https://doi.org/10.5194/acp-22-823-2022
https://doi.org/10.5194/acp-22-823-2022
Research article
 | 
18 Jan 2022
Research article |  | 18 Jan 2022

Box model trajectory studies of contrail formation using a particle-based cloud microphysics scheme

Andreas Bier, Simon Unterstrasser, and Xavier Vancassel

Related authors

Contrail formation on ambient aerosol particles for aircraft with hydrogen combustion: a box model trajectory study
Andreas Bier, Simon Unterstrasser, Josef Zink, Dennis Hillenbrand, Tina Jurkat-Witschas, and Annemarie Lottermoser
Atmos. Chem. Phys., 24, 2319–2344, https://doi.org/10.5194/acp-24-2319-2024,https://doi.org/10.5194/acp-24-2319-2024, 2024
Short summary

Related subject area

Subject: Clouds and Precipitation | Research Activity: Atmospheric Modelling and Data Analysis | Altitude Range: Troposphere | Science Focus: Physics (physical properties and processes)
High-resolution modeling of early contrail evolution from hydrogen-powered aircraft
Annemarie Lottermoser and Simon Unterstrasser
Atmos. Chem. Phys., 25, 7903–7924, https://doi.org/10.5194/acp-25-7903-2025,https://doi.org/10.5194/acp-25-7903-2025, 2025
Short summary
Accelerated impact of airborne glaciogenic seeding of stratiform clouds by turbulence
Meilian Chen, Xiaoqin Jing, Jiaojiao Li, Jing Yang, Xiaobo Dong, Bart Geerts, Yan Yin, Baojun Chen, Lulin Xue, Mengyu Huang, Ping Tian, and Shaofeng Hua
Atmos. Chem. Phys., 25, 7581–7596, https://doi.org/10.5194/acp-25-7581-2025,https://doi.org/10.5194/acp-25-7581-2025, 2025
Short summary
Failed cyclogenesis of a mesoscale convective system near Cabo Verde: the role of the Saharan trade wind layer among other inhibiting factors observed during the CADDIWA field campaign
Guillaume Feger, Jean-Pierre Chaboureau, Thibaut Dauhut, Julien Delanoë, and Pierre Coutris
Atmos. Chem. Phys., 25, 7447–7465, https://doi.org/10.5194/acp-25-7447-2025,https://doi.org/10.5194/acp-25-7447-2025, 2025
Short summary
Sensitivities of simulated mixed-phase Arctic multilayer clouds to primary and secondary ice processes
Gabriella Wallentin, Annika Oertel, Luisa Ickes, Peggy Achtert, Matthias Tesche, and Corinna Hoose
Atmos. Chem. Phys., 25, 6607–6631, https://doi.org/10.5194/acp-25-6607-2025,https://doi.org/10.5194/acp-25-6607-2025, 2025
Short summary
Assessing glaciogenic seeding impacts in Australia's Snowy Mountains: an ensemble modeling approach
Sisi Chen, Lulin Xue, Sarah A. Tessendorf, Thomas Chubb, Andrew Peace, Suzanne Kenyon, Johanna Speirs, Jamie Wolff, and Bill Petzke
Atmos. Chem. Phys., 25, 6703–6724, https://doi.org/10.5194/acp-25-6703-2025,https://doi.org/10.5194/acp-25-6703-2025, 2025
Short summary

Cited articles

Agarwal, A., Speth, R., Fritz, T., Jacob, S., Rindlisbacher, T., Iovinelli, R., Owen, B., Miake-Lye, R., Sabnis, J., and Barrett, S.: SCOPE11 method for estimating aircraft black carbon mass and particle number emissions, Environ. Sci. Technol., 53, 1364–1373, https://doi.org/10.1021/acs.est.8b04060, 2019. a
Anderson, E. B., Cofer, R. W., Bagwell, D. R., Barrick, J. W., Hudgins, C. H., and Brunke, K. E.: Airborne observations of aircraft aerosol emissions 1,Total nonvolatile particle emission indices, Geophys. Res. Lett., 25, 1689–1692, 1998. a
Barrett, J. C. and Clement, C. F.: Growth rates for liquid drops, J. Aerosol Sci., 19, 223–242, https://doi.org/10.1016/0021-8502(88)90225-X, 1988. a
Bier, A. and Burkhardt, U.: Variability in Contrail Ice Nucleation and Its Dependence on Soot Number Emissions, J. Geophys. Res., 124, 3384–3400, https://doi.org/10.1029/2018JD029155, 2019. a, b, c, d
Bier, A., Burkhardt, U., and Bock, L.: Synoptic Control of Contrail Cirrus Life Cycles and Their Modification Due to Reduced Soot Number Emissions, J. Geophys. Res., 122, 11584–11603, https://doi.org/10.1002/2017JD027011, 2017JD027011, 2017. a
Download
Short summary
We investigate contrail formation in an aircraft plume with a particle-based multi-trajectory 0D model. Due to the high plume heterogeneity, contrail ice crystals form first near the plume edge and then in the plume centre. The number of ice crystals varies strongly with ambient conditions and soot properties near the contrail formation threshold. Our results imply that the multi-trajectory approach does not necessarily lead to improved scientific results compared to a single mean trajectory.
Share
Altmetrics
Final-revised paper
Preprint