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https://pubs.acs.org/doi/abs/10.1021/acs.est.3c04793

*Authors*
Diana C. Hernandez-Jaramillo*, Luke Harrison, Brendan Kelaher, Zoran
Ristovski, and Daniel P. Harrison

*Publication Date: November 29, 2023*

https://doi.org/10.1021/acs.est.3c04793

*Abstract*
Marine cloud brightening (MCB) is a potential intervention to mitigate the
effects of climate change by increasing the reflectance of low-level
maritime clouds, including those over the Great Barrier Reef. The technique
involves dispersing a plume of submicrometer seawater droplets over the
ocean, which evaporate, generating nanosized sea-salt aerosols (SSAs) that
disperse through the atmosphere with some fraction incorporated into
clouds. Droplet evaporation, which occurs in the immediate vicinity (meters
to tens of meters) of the source, has been theorized to produce a
negatively buoyant plume hindering the mixing of the sea-salt aerosol to
cloud height and compromising the effectiveness of MCB. We characterized in
situ for the first time the nearfield aerosol dispersion from a point
source of atomized seawater produced using the effervescent technique. We
observed consistent vertical mixing of the plume up to 150 ± 5 m height at
1 km downwind. The extent of vertical dispersion was influenced by wind
velocity and atmospheric stability. We found no evidence that negative
buoyancy due to the evaporation of the 0.068 kg/s water fraction
significantly suppressed vertical mixing. Our results can be attributed to
the small droplet sizes generated by the effervescent spray technology and
associated low flow rates required to generate around 1014 droplets s–1. We
estimate that, for a hypothetical implementation producing up to 1016 s–1
similarly sized SSAs, evaporative cooling is unlikely to significantly
suppress the vertical dispersion of aerosol for MCB.
[image: Abstract Image]*Source: ACS PUBLICATIONS*

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