The Effect of Planetary Rotation Period on Clouds in a Global Climate Model with a Bin Microphysics Scheme
Huanzhou Yang, Eric T. Wolf, Cheng-Cheng Liu, Yunqian Zhu, Owen B. Toon, and Dorian S. Abbot

TL;DR
This study compares a size-resolved bin microphysics model with a traditional parameterized scheme in a climate model to assess cloud differences on exoplanets with varying rotation rates, impacting climate and observational interpretations.
Contribution
It demonstrates the differences between bin microphysics and parameterized schemes in exoplanet climate simulations, highlighting the importance of resolved microphysics for accurate cloud representation.
Findings
CARMA produces fewer liquid clouds and more ice clouds than MG
Ice cloud size distribution differs significantly, affecting spectral retrievals
Net cloud radiative effect decreases by 4-10 W/m^2
Abstract
Clouds are the largest source of uncertainty in climate simulations. For exoplanets, cloud simulation is particularly challenging because of the lack of observational data to tune parameterized cloud models. Here we apply Community Aerosol and Radiation Model for Atmospheres (CARMA), a size-resolved bin cloud microphysics model, to the atmospheric global climate model Community Atmosphere Model (CAM6) and simulate exoplanets with a range of planetary rotation rates. CARMA produces fewer liquid clouds than the native CAM6 parameterized cloud microphysics scheme (Morrison-Gettelman two-moment microphysics, MG), more ice clouds, and a significantly different ice cloud size distribution. Overall, this leads to a decrease in the magnitude of the net CRE by 4-10 , which is unlikely to change the determination of habitability from a climate perspective in most cases. The difference in…
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Taxonomy
TopicsStellar, planetary, and galactic studies · Astronomy and Astrophysical Research · Astrophysics and Star Formation Studies
