https://iopscience.iop.org/article/10.1088/1748-9326/adccd7/meta

*Authors*
Diana Carolina Hernandez Jaramillo, Luke Harrison, Grace Gunner, Andrew
McGrath, Wolfgang Junkermann, Wolfgang Lieff, Jorg Hacker, Daniel
Rosenfeld, Brendan Kelaher and Daniel P. Harrison

Accepted Manuscript online *15 April 2025*

*Abstract*
Regional scale Marine Cloud Brightening (MCB) has been proposed as a novel
climate intervention to reduce the impact of global warming and associated
marine heatwaves on the
Great Barrier Reef (GBR). The concept relies on
artificially generated sea spray aerosols (SSA) at the ocean surface and
their transport in sufficient quantities to low-level maritime clouds. A
portion of the SSA that reaches cloud height can act as additional cloud
condensation nuclei and modify cloud microphysical properties, potentially
reducing the amount of solar radiation reaching the sea surface. Although
modelling data supports the MCB concept, field experiments demonstrating
the dispersion of artificially produced sea spray aerosols to clouds have
not been previously reported. Here, we show that within a field of
low-level trade wind cumulus-type clouds, an aerosol plume generated at the
sea surface on board a research vessel was rapidly advected to cloud base
height. Aircraft measurements conducted during two different sampling
strategies, detected the aerosol plume from the vessel's sea water
atomisation system just below cloud bases at 700–900 m altitudes. For an
estimated surface level aerosol production rate of 4 × 1014/s, aerosol
concentrations at cloud base were detected with peak number concentrations
of up to ~1 × 103/cm3. Although such production rates of aerosol particles
are orders of magnitude less than what is envisioned for any practical
implementation of MCB, our results indicate that cloud perturbation
experiments should now be possible using surface-produced sea spray
aerosols.

*Source: IOP Science*

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