- 1School of Physical and Chemical Sciences, University of Canterbury, Christchurch, New Zealand (laura.revell@canterbury.ac.nz)
- 2Physikalisch-Meteorologisches Observatorium Davos and World Radiation Center, Davos, Switzerland
- 3Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland
- 4John A. Paulson School of Engineering and Applied Sciences, Harvard University, Cambridge, MA, USA
- 5Department of Mechanical Engineering, University of Canterbury, Christchurch, New Zealand
- 6Instituto de Geociencias (IGEO), CSIC-UCM, Madrid, Spain
Rocket emissions damage the stratospheric ozone layer, which protects life from harmful solar radiation. To understand if significant ozone losses could occur as the launch industry grows, we examine two scenarios of industry aspirations. Our ‘ambitious’ scenario (2,040 launches/year) leads to a -0.29% depletion in annual-mean, near-global total column ozone, relative to a simulation with no rocket launches. Antarctic springtime ozone decreases by 3.9%. Our ‘conservative’ scenario (884 launches/year) leads to a -0.17% annual depletion; current licensing rates suggest this scenario may be exceeded sooner than 2030. Ozone losses are mostly driven by the reactive chlorine produced from solid rocket motor propellant, and black carbon which is emitted from most propellants in contemporary use. The ozone layer is slowly healing from the effects of anthropogenic CFCs, yet ozone abundances are still 2% lower than those measured prior to the onset of CFC-induced ozone depletion. Our results demonstrate that ongoing and frequent rocket launches could delay ozone recovery. Action is needed now to ensure that future growth of the launch industry and ozone protection are mutually sustainable.
How to cite: Revell, L., Bannister, M., Brown, T., Sukhodolov, T., Vattioni, S., Dykema, J., Frame, D., Cater, J., Chiodo, G., and Rozanov, E.: Near-future rocket launches could slow ozone recovery, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-1201, https://doi.org/10.5194/egusphere-egu25-1201, 2025.