https://egusphere.copernicus.org/preprints/2023/egusphere-2023-1720/

*Authors*
Prasanth Prabhakaran <[email protected]>, Fabian Hoffmann, and Graham
Feingold
*Received: 26 Jul 2023 – Discussion started: 17 Aug 2023*

Abstract. We explore the role of intermittent aerosol forcing (e.g., ship
tracks, or injections associated with marine cloud brightening) on the
stratocumulus-to-cumulus transition (SCT). We simulate a three-day
Lagrangian trajectory in the north-east Pacific using a large-eddy
simulation model coupled to a bin-emulating, two-moment, bulk microphysics
scheme that captures the evolution of aerosol and cloud droplet
concentrations. By varying the background aerosol concentration, we
consider two baseline systems - pristine and polluted. We perturb the
baseline cases with a range of aerosol injection strategies by varying the
injection rate, number of injectors, and the timing of the aerosol
injection. Our results show that aerosol dispersal is more efficient under
pristine conditions due to a transverse circulation created by the
gradients in precipitation rates across the plume track. Furthermore, we
see that a substantial enhancement in the cloud radiative effect (CRE) is
evident in both systems. In the polluted system, the albedo effect (smaller
but more numerous droplets causing brighter clouds at constant liquid
water) is the dominant contributor in the initial two days. The
contributions from liquid water path (LWP) and cloud fraction adjustments
are important on the third and fourth day, respectively. In the pristine
system, cloud fraction adjustments are the dominant contributor to the CRE
on all three days, followed by the albedo effect. In both these systems, we
see that the SCT is delayed due to the injection of aerosol, and the extent
of the delay is proportional to the number of particles injected into the
marine boundary layer.
How to cite. Prabhakaran, P., Hoffmann, F., and Feingold, G.: Effects of
Intermittent Aerosol Forcing on the Stratocumulus-to-Cumulus Transition,
EGUsphere [preprint], https://doi.org/10.5194/egusphere-2023-1720, 2023.
*Source: EGUsphere*

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