Implications of smaller concentrations of stratospheric OH: A two-dimensional model study of ozone perturbations

Abstract

There is growing observational evidence that stratospheric OH concentrations are smaller than models have been predicting. Using very recent HO x reaction rate coefficient measurements in a two-dimensional photochemical model, results which support these observations are obtained. As a consequence of smaller OH concentrations, we show that perturbations of stratospheric ozone by NO x (SST emissions and nitrogen fertilizers) may be larger than expected, while perturbations due to added water vapor and chlorine (SSTs and chlorofiuoromethanes. respectively) may be smaller.