In this second part of a series of articles dedicated to a detailed analysis of bromine chemistry in the atmosphere we address one (out of two) dominant natural sources of reactive bromine. The two main source categories are the release of bromine from sea salt and the decomposition of bromocarbons by photolysis and reaction with OH. Here, we focus on C<sub>1</sub>-bromocarbons. We show that the atmospheric chemistry general circulation model ECHAM5/MESSy realistically simulates their emission, transport and decomposition from the boundary layer up to the mesosphere. We included oceanic emission fluxes of the short-lived bromocarbons CH<sub>2</sub>Br<sub>2</sub>, CH<sub>2</sub>ClBr, CHClBr<sub>2</sub>, CHCl<sub>2</sub>Br, CHBr<sub>3</sub> and of CH<sub>3</sub>Br. The vertical profiles and the surface mixing ratios of the bromocarbons are in general agreement with the (few available) observations, especially in view of the limited information available and the consequent coarseness of the emission fields. For CHBr<sub>3</sub>, CHCl<sub>2</sub>Br and CHClBr<sub>2</sub> photolysis is the most important degradation process in the troposphere. In contrast to this, tropospheric CH<sub>2</sub>Br<sub>2</sub>, CH<sub>3</sub>Br and CH<sub>2</sub>ClBr are more efficiently decomposed by reaction with OH. In the free troposphere approximately 40% of the C<sub>1</sub>-bromocarbons decompose by reaction with OH. Our results indicate that bromoform contributes substantial amounts of reactive bromine to the lower stratosphere and thus should not be neglected in stratospheric simulations
