EGU21-5732
https://doi.org/10.5194/egusphere-egu21-5732
EGU General Assembly 2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

How much variability in upper tropospheric cloud-radiative heating can be attributed to ice microphysics?

Sylvia Sullivan1, Aiko Voigt2, Annette Miltenberger3, Christian Rolf4, and Martina Krämer3,4
Sylvia Sullivan et al.
  • 1Institute for Meteorology and Climate Research, Karlsruhe Institute of Technology, Karlsruhe, Germany (sylvia.sullivan@kit.edu)
  • 2Department of Meteorology and Geophysics, University of Vienna, Vienna, Austria (aiko.voigt@univie.ac.at)
  • 3Institute for Atmospheric Physics, Johannes Gutenberg-Universität Mainz, Mainz, Germany (amiltenb@uni-mainz.de)
  • 4Forschungszentrum Jülich, Jülich, Germany (c.rolf@fz-juelich.de, m.kraemer@fz-juelich.de)

While large-domain simulations without convective parameterization are now computationally feasible, microphysics, particularly that of the ice phase, remains a persistent problem for high-resolution models. In 2.5-km equivalent resolution simulations with the ICON model, we find that switching between one- and two-moment ice microphysics can alter cloud top cooling by a factor of ten and in-cloud heating by a factor of four above 350 hPa. A consistent ice crystal effective radius between microphysics and radiation increases the cloud-radiative heating another two-fold, while inclusion of aerosol-cloud interactions reduces it at lower levels between 400 and 500 hPa. We also generate 60-hour trajectories from ICON within ice clouds and use them to force a detailed ice microphysics box model, the Chemical Lagrangian Model of the Stratosphere (ClaMs-ice). We compare the ice mass and number tendencies, as well as the sedimentation fluxes, between ICON and CLaMS-ice. These offline simulations also allow us to quantify the strength of microphysical-radiative feedbacks and investigate the impact on heating of particular ice microphysical factors, including gravity wave parameterization, ice-nucleating particle concentrations, and the number concentration of solution droplets.

How to cite: Sullivan, S., Voigt, A., Miltenberger, A., Rolf, C., and Krämer, M.: How much variability in upper tropospheric cloud-radiative heating can be attributed to ice microphysics?, EGU General Assembly 2021, online, 19–30 Apr 2021, EGU21-5732, https://doi.org/10.5194/egusphere-egu21-5732, 2021.

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