Skip to main content
. Author manuscript; available in PMC: 2020 Aug 11.
Published in final edited form as: Photochem Photobiol Sci. 2019 Feb 27;18(3):747–774. doi: 10.1039/c8pp90063a

Fig. 5.

Fig. 5

Schematic illustration of the formation of halocarbons in seawater that undergo UV-induced reactions in the troposphere yielding reactive halogen species such as bromine monoxide (BrO) that act as oxidants for atmospheric pollutants, e.g., gaseous elementary mercury (Hg0g). Brominated very-short-lived substances (BrVSLS) may reach the lowermost stratosphere and participate in stratospheric ozone depletion.