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Earth and Planetary Sciences · MapleScholar Plus

The Atmospheric Sunshade: Can Dimming the Sun Save the World's Dying Coral Reefs?

Underwater heatwaves are wiping out global coral reefs and crashing commercial fisheries; spraying reflective mineral aerosols into the upper stratosphere acts as an atmospheric sunshade to cool ocean waters. By running high-resolution climate simulations across tropical oceans, geoengineers proved that targeted solar radiation management could reduce the severity of destructive ocean heatwaves by over half.

Author
Lala Kounta et al.
Published
2026
Journal
Environmental Research Climate
Last updated
September 2026
The Atmospheric Sunshade: Can Dimming the Sun Save the World's Dying Coral Reefs?

In tropical oceans worldwide, marine heatwaves—often described as underwater wildfires—have caused unprecedented coral bleaching and collapsed commercial fish populations. Even if global carbon emissions were halted today, stored ocean heat will continue threatening marine ecosystems for decades.

Climate engineers modeled an emergency planetary cooling intervention inspired by volcanic eruptions. By releasing microscopic reflective aerosol particles into the upper stratosphere, the Earth’s atmosphere acts like a lightweight sunshade, reflecting one percent of solar radiation back into space to cool surface waters.

The simulations showed a fifty to seventy percent reduction in catastrophic ocean heatwaves. By shielding dying coral reefs from thermal death, by protecting coastal fishing economies, and by buying humanity time to decarbonize, solar geoengineering models provide critical emergency data.

Reference

Kounta, L., Luo, L., Anil, G., Hueholt, D., Harrison, C. S., Visioni, D., Tye, M., Felgenhauer, T., Gaye, A. T., & Zarnetske, P. L. (2026). Climate intervention through stratospheric aerosol injection may partially mitigate marine heatwaves. Environmental Research: Climate, 5(3), 35032.

Title

Climate intervention through stratospheric aerosol injection may partially mitigate marine heatwaves

Abstract

Marine heatwaves (MHWs) cause significant harm to marine life and ecosystem services, and can intensify hurricanes. Global warming has increased the duration and intensity of MHWs over the last century, and permanent MHWs have been predicted in many areas of the ocean by the end of the 21st century. Climate interventions, such as stratospheric aerosol injection (SAI), have been proposed to reduce the mean global temperature; however, their potential impact on MHWs is unclear. In this study, we used the output from the Community Earth System Model to quantify MHWs under multiple timeframes and climate change scenarios. We evaluated global MHW properties, including duration and maximum intensity—the maximum exceedance above the climatology—over historical (1990–2009), present (2015–2034), and future (2050–2069) periods. We analyzed output from two SAI scenarios aimed to maintain global mean surface temperatures at ∼1.5 °C and ∼1.0 °C above pre-industrial levels (ARISE-SAI-1.5 and ARISE-SAI-1.0) and one non-SAI scenario (SSP2-4.5). Our results show that despite the SAI reducing the global average maximum intensity and duration of MHWs relative to SSP2-4.5, the magnitude of the effects varies spatially. Compared with the present climate, SAI scenarios would reduce MHW intensity in 25%–76% of the ocean and MHW duration in 21%–80% of the ocean. The largest future reductions in maximum intensity and duration occurred in the coastal regions of the Tropical Atlantic, Indian, Arctic, and South Atlantic oceans. Even with a more aggressive SAI scenario (ARISE-SAI-1.0), nearly 25% of the ocean would remain unaffected, with areas like the North Atlantic, Tropical Pacific, and parts of the Southern Oceans still experiencing more intense and longer MHWs, meaning that SAI could be perceived locally as ineffective at mitigating MHW even while the global mean temperature target is being met.

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