The relative effectiveness of bromine compared to chlorine for destroying s
tratospheric ozone is explored. Two definitions previously used to quantify
this relative effectiveness, typically referred to as alpha, are compared
and a definition is presented to calculate alpha values applicable for colu
mn and global ozone loss. Calculations of alpha are made with a two-dimensi
onal radiative/chemical/dynamical model and suggest that bromine is roughly
45 times more effective than chlorine for global ozone destruction. The ph
ysical processes underlying this result are probed, and sensitivity studies
are presented that show that relatively large changes invoked in the model
ed transport and heterogeneous chemistry lead to changes in this value of <
15%.