Frequent and severe bleaching under global warming has resulted in widespread coral mortality and decline across the globe. To prevent further decline of reefs, warming needs to be limited to 1.5℃ or below, which requires rapid emission reduction that is yet to be achieved. Solar climate intervention (SCI) is being considered as a supplement to emission reductions and other risk mitigation strategies to prevent exceeding climate tipping points. However, there is a crucial need to investigate impacts to ecosystems to inform scenario development and decision-making. Here, we use daily sea surface temperature (SST) data from the Community Earth System Model simulations to project and compare thermal coral bleaching under a moderate emissions scenario, SSP2-4.5, with and without intervention using stratospheric aerosol injection (SAI). To understand the impact of temperature targets and timing of deployment on coral thermal bleaching, we use three SAI scenarios: SAI-1.0, starting in 2035 and limiting warming to 1.0℃, SAI-1.5, starting in 2035 and limiting warming to 1.5℃, and SAI-Delayed starting in 2045 and limiting warming to ~1.37℃. We found that under all three SAI scenarios, global reef provinces experience significantly lower levels of thermal stress relative to SSP2-4.5. Among the three intervention scenarios, SAI limiting warming to 1.0℃ in 2035 most effectively mitigates thermal bleaching over space and time.
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Kicking the can down the road: understanding the effects of delaying the deployment of stratospheric aerosol injection
Abstract Climate change is a prevalent threat, and it is unlikely that current mitigation efforts will be enough to avoid unwanted impacts. One potential option to reduce climate change impacts is the use of stratospheric aerosol injection (SAI). Even if SAI is ultimately deployed, it might be initiated only after some temperature target is exceeded. The consequences of such a delay are assessed herein. This study compares two cases, with the same target global mean temperature of ∼1.5° C above preindustrial, but start dates of 2035 or a ‘delayed’ start in 2045. We make use of simulations in the Community Earth System Model version 2 with the Whole Atmosphere Coupled Chemistry Model version 6 (CESM2-WACCM6), using SAI under the SSP2-4.5 emissions pathway. We find that delaying the start of deployment (relative to the target temperature) necessitates lower net radiative forcing (−30%) and thus larger sulfur dioxide injection rates (+20%), even after surface temperatures converge, to compensate for the extra energy absorbed by the Earth system. Southern hemisphere ozone is higher from 2035 to 2050 in the delayed start scenario, but converges to the same value later in the century. However, many of the surface climate differences between the 2035 and 2045 start simulations appear to be small during the 10–25 years following the delayed SAI start, although longer simulations would be needed to assess any longer-term impacts in this model. In addition, irreversibilities and tipping points that might be triggered during the period of increased warming may not be adequately represented in the model but could change this conclusion in the real world.
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- Award ID(s):
- 1754740
- PAR ID:
- 10553749
- Publisher / Repository:
- Institute of Physics
- Date Published:
- Journal Name:
- Environmental Research: Climate
- Volume:
- 3
- Issue:
- 3
- ISSN:
- 2752-5295
- Page Range / eLocation ID:
- 035011
- Format(s):
- Medium: X
- Sponsoring Org:
- National Science Foundation
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