The climate crisis, characterized by atmospheric COâ‚‚ concentrations exceeding 420 ppm, and persistent stratospheric ozone depletion necessitate integrated mitigation strategies that address multiple dimensions of atmospheric degradation simultaneously. While artificial carbon capture technologies have emerged as critical interventions for achieving net-zero emissions and the Montreal Protocol has successfully initiated ozone layer recovery, the potential synergies and trade-offs between these atmospheric interventions remain inadequately understood, particularly regarding how large-scale carbon removal deployment might influence stratospheric chemistry and ozone recovery trajectories.