An overshoot of the 1.5°C benchmark would have serious consequences. For example, the melting of the ice sheets on Greenland and in the Antarctic would be virtually unstoppable, which would cause sea levels to rise in the long-term. The risk of extreme weather events such as droughts and heatwaves would also increase.
It would theoretically be possible to achieve a lowering back to below 1.5°C even after an overshoot. This would require enormous efforts and, in addition to the already necessary strengthening of natural CO2 sinks such as forests, the large-scale use of carbon capture and storage technologies. These technologies, which remove CO2 from the atmosphere and store it in e.g. geological formations are currently only available on a small scale. They are extremely expensive, resource-intensive and their potential impact on the environment is not (yet) foreseeable.
It is therefore important to keep the global temperature increase as low as possible: Every temperature increase that is avoided, however small, counts. A temporary overshoot of the 1.5°C benchmark must be minimised in extent and duration. Any overshoot can result in serious and potentially irreversible changes in the climate system, with unforeseeable effects on people and the environment. The premise therefore remains to act early and consistently in order to avoid such scenarios.