Preprints
https://doi.org/10.5194/egusphere-2025-3708
https://doi.org/10.5194/egusphere-2025-3708
04 Sep 2025
 | 04 Sep 2025
Status: this preprint is open for discussion and under review for Atmospheric Chemistry and Physics (ACP).

Contrail formation for aircraft with hydrogen combustion – Part 2: Engine-related aspects

Josef Zink and Simon Unterstrasser

Abstract. The number of ice crystals formed in nascent contrails strongly influences contrail-cirrus life cycle and radiative forcing. Previous studies on contrails from hydrogen combustion focused on microphysical processes that affect the ice crystal number. These studies, however, paid less attention to engine-related aspects. To fill this gap, we investigate how the exhaust plume evolution is thermodynamically influenced by (i) the engine's overall propulsion efficiency, (ii) the engine exit conditions due to varying ambient conditions, (iii) the engine size and exit jet speed, and (iv) the explicit treatment of kinetic energy dissipation and entrainment of enthalpy initially contained in the bypass flow of a turbofan engine. Based on simulations with the box model version of the Lagrangian Cloud Module, we investigate how these aspects influence the contrail formation process and derive suitable (scaling) relations for the number of ice crystals formed Nice,f on entrained ambient aerosols for hydrogen combustion. These relations help to derive an expression of Nice,f through a functional relationship that relies on a reduced set of input parameters, while ensuring a generalized parametrization of Nice,f in contrails from hydrogen combustion.

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Josef Zink and Simon Unterstrasser

Status: open (until 16 Oct 2025)

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Josef Zink and Simon Unterstrasser
Josef Zink and Simon Unterstrasser

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Short summary
The climate impact of aviation-induced contrail cirrus clouds is strongly influenced by the number of ice crystals that form in the wake of an aircraft under certain conditions. In this study, we investigate how engine-related aspects influence the number of ice crystals formed for hydrogen combustion. We derive suitable (scaling) relations that can be integrated into large-scale models used to estimate the climate impact of contrail cirrus clouds.
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