https://egusphere.copernicus.org/preprints/2025/egusphere-2025-2935/

*Authors*
Prasanth Prabhakaran, Timothy A. Myers, Fabian Hoffmann, and Graham Feingold

*Received: 20 Jun 2025 – Discussion started: 27 Jun 2025*

*Abstract*
We explore the impact of aerosol perturbation on the
stratocumulus-to-cumulus transition (SCT) in a warmer climate in the
North-East Pacific region using a Lagrangian large-eddy simulation model
coupled to a two-moment, bin-emulating bulk microphysics scheme. We explore
two SCT cases with different free-tropospheric (FT) humidities – moist FT
and dry FT. For each case, we consider two Shared Socioeconomic Pathways
(SSPs), SSP3-7.0 and SSP1-2.6, from the most recent Coupled Model
Intercomparison Project (CMIP6) to determine the extent of warming and
changes in aerosol concentration at the end-of-the-century. We find that
the cloud radiative effect (CRE) in non-precipitating stratocumulus clouds
is more susceptible to climate change than to aerosol. However, after the
breakup of the cloud deck, the impact of aerosol tends to dominate.
Furthermore, in these low-clouds, aerosol-cloud interactions (Twomey effect
and liquid water path adjustments) are to leading order immune to climate
change, unless aerosol-induced cloud fraction adjustment is significant. We
extend the analysis to marine cloud brightening and show that its efficacy
decreases with warming because of the reduction in cloud fraction. We also
explore the impact of climate change and aerosol perturbation on SCT. In
the moist FT case, climate change advances the onset of cumulus activity
and cloud breakup. However, in the dry FT case, climate change does not
affect the onset of cumulus activity but delays cloud breakup. In both
cases, aerosol injection delays cloud breakup via precipitation suppression
but does not affect cumulus onset unless it is coupled to rain formation.

*Source: EGUsphere*

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