EGU25-9491, updated on 14 Mar 2025
https://doi.org/10.5194/egusphere-egu25-9491
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Tuesday, 29 Apr, 08:30–10:15 (CEST), Display time Tuesday, 29 Apr, 08:30–12:30
 
Hall X5, X5.60
Simulation of radiatively driven mixing in a smoke cloud using "one-dimensional turbulence"
Hanchen Li1,2, Marten Klein1,2, and Heiko Schmidt1,2
Hanchen Li et al.
  • 1Numerical Fluid and Gas Dynamics, Brandenburg University of Technology Cottbus-Senftenberg, Cottbus, Germany
  • 2Scientific Computing Lab, Energy Innovation Center (EIZ) Cottbus, Germany

Large-eddy simulations (LESs) are known to significantly overestimate entrainment in cloud-topped boundary layers, negatively impacting predictions on cloud mass and cover. This overestimation stems from coarse model resolutions that lead to numerical broadening of the entrainment layer. While it has been shown in direct numerical simulations (DNSs) that down-to-centimetre-scale resolutions can mitigate this issue, such high resolutions are not viable for most applications in the atmospheric sciences. The one-dimensional turbulence model (ODT), introduced by Kerstein [1], offers a computationally efficient alternative that provides full-scale resolution along a 1-D vertical domain. Molecular diffusion is explicitly resolved, while turbulent advection is modelled through a stochastically sampled sequence of spatial mappings, known as eddy events. Physically plausible eddy events are selected based on their current kinetic and potential energy. This allows an accurate representation of local turbulence properties and their dynamical complexity by evolving instantaneous property profiles. This study applies ODT to investigate cloud-top turbulent mixing processes driven by radiative cooling in a smoke cloud, benchmarking the results against DNS. Building on the preliminary findings by Meiselbach [2], we demonstrate improvements in mean profiles and turbulent fluxes of buoyancy and smoke concentration, showing ODT's ability to reproduce salient features observed in DNSs. In addition, we explore convective boundary layer scalings at extended Reynolds and Richardson numbers beyond those accessible in DNS studies.
 

References:
[1] A. R. Kerstein, Journal of Fluid Mechanics 392, 277334 (1999).
[2] F. T. Meiselbach, Application of ODT to Turbulent Flow Problems, doctoral thesis, BTU Cottbus-Senftenberg (2015).

How to cite: Li, H., Klein, M., and Schmidt, H.: Simulation of radiatively driven mixing in a smoke cloud using "one-dimensional turbulence", EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-9491, https://doi.org/10.5194/egusphere-egu25-9491, 2025.