Articles | Volume 19, issue 20
https://doi.org/10.5194/gmd-19-10185-2026
https://doi.org/10.5194/gmd-19-10185-2026
Model description paper
 | 
27 Oct 2026
Model description paper |  | 27 Oct 2026

Stochastic homogeneous freezing of supercooled droplets in mixed-phase clouds in particle-based idealised microphysics framework (exemplified with PySDM v3.0)

Tim Lüttmer, Sylwester Arabas, and Peter Spichtinger

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Cited articles

Abade, G. C. and Albuquerque, D. G.: Persistent mixed-phase states in adiabatic cloud parcels under idealised conditions, Q. J. Roy. Meteor. Soc., 150, 3450–3474, https://doi.org/10.1002/qj.4775, 2024. a
Alpert, P. A. and Knopf, D. A.: Analysis of isothermal and cooling-rate-dependent immersion freezing by a unifying stochastic ice nucleation model, Atmos. Chem. Phys., 16, 2083–2107, https://doi.org/10.5194/acp-16-2083-2016, 2016. a
Arabas, S., Jaruga, A., Pawlowska, H., and Grabowski, W. W.: libcloudph++ 1.0: a single-moment bulk, double-moment bulk, and particle-based warm-rain microphysics library in C++, Geosci. Model Dev., 8, 1677–1707, https://doi.org/10.5194/gmd-8-1677-2015, 2015. a
Arabas, S., Curtis, J. H., Silber, I., Fridlind, A. M., Knopf, D. A., West, M., and Riemer, N.: Immersion Freezing in Particle-Based Aerosol-Cloud Microphysics: A Probabilistic Perspective on Singular and Time-Dependent Models, J. Adv. Model. Earth Sy., 17, https://doi.org/10.1029/2024MS004770, 2025. a, b
Bartman, P., Bulenok, O., Górski, K., Jaruga, A., Łazarski, G., Olesik, M. A., Piasecki, B., Singer, C. E., Talar, A., and Arabas, S.: PySDM v1: particle-based cloud modeling package for warm-rain microphysics and aqueous chemistry, Journal of Open Source Software, 7, 3219, https://doi.org/10.21105/joss.03219, 2022. a
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Short summary
Homogeneous freezing describes the spontaneous freezing of supercooled droplets, with the probability depending on temperature, droplet size, and elapsed time. Droplets freeze across a range of temperatures rather than all at once, and faster updrafts and larger droplets lead to freezing at warmer temperatures. Once some droplets freeze, the growing ice crystals deplete the surrounding vapour, causing the remaining droplets to evaporate. This affects the number of ice crystals in the cloud.
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