https://www.nature.com/articles/s41561-024-01427-z


*Authors*
Ying Chen, Jim Haywood, Yu Wang, Florent Malavelle, George Jordan, Amy
Peace, Daniel G. Partridge, Nayeong Cho, Lazaros Oreopoulos, Daniel
Grosvenor, Paul Field, Richard P. Allan & Ulrike Lohmann

*11 April 2024*

*Citations*: Chen, Y., Haywood, J., Wang, Y. et al. Substantial cooling
effect from aerosol-induced increase in tropical marine cloud cover. Nat.
Geosci. (2024). https://doi.org/10.1038/s41561-024-01427-z

*Abstract*
With global warming currently standing at approximately +1.2 °C since
pre-industrial times, climate change is a pressing global issue. Marine
cloud brightening is one proposed method to tackle warming through
injecting aerosols into marine clouds to enhance their reflectivity and
thereby planetary albedo. However, because it is unclear how aerosols
influence clouds, especially cloud cover, both climate projections and the
effectiveness of marine cloud brightening remain uncertain. Here we use
satellite observations of volcanic eruptions in Hawaii to quantify the
aerosol fingerprint on tropical marine clouds. We observe a large
enhancement in reflected sunlight, mainly due to an aerosol-induced
increase in cloud cover. This observed strong negative aerosol forcing
suggests that the current level of global warming is driven by a weaker net
radiative forcing than previously thought, arising from the competing
effects of greenhouse gases and aerosols. This implies a greater
sensitivity of Earth’s climate to radiative forcing and therefore a larger
warming response to both rising greenhouse gas concentrations and
reductions in atmospheric aerosols due to air quality measures. However,
our findings also indicate that mitigation of global warming via marine
cloud brightening is plausible and is most effective in humid and stable
conditions in the tropics where solar radiation is strong.

Aerosol fingerprints on clouds from natural experiments.
[image: figure 2]
<https://www.nature.com/articles/s41561-024-01427-z/figures/2>
Conceptual model of cloud cover’s response to aerosol perturbation.
[image: figure 4]
<https://www.nature.com/articles/s41561-024-01427-z/figures/4>

*Source: nature geosciences*

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