Composite global emissions of reactive chlorine from anthropogenic and natural sources: Reactive Chlorine Emissions Inventory

Emission inventories for major reactive tropospheric Cl species (particulat e Cl, HCl, ClNO2, CH3Cl, CHCl3, CH3CCl3, C2Cl4, C2HCl3, CH2Cl2 and CHClF2) were integrated across source types (terrestrial biogenic and oceanic emiss ions, sea-salt production and dechlorination, biomass burning, industrial e missions, fossil-fuel combustion, and incineration). Composite emissions we re compared with known sinks to assess budget closure; relative contributio ns of natural and anthropogenic sources were differentiated. Model calculat ions suggest that conventional acid-displacement reactions involving S-(IV) +O-3, S-(IV)+ H2O2, and H2SO4 and HNO3 scavenging account for minor fractio ns of sea-salt dechlorination globally. Other important chemical pathways i nvolving sea-salt aerosol apparently produce most volatile chlorine in the troposphere. The combined emissions of CH3Cl from known sources account for about half of the modeled sink, suggesting fluxes from known sources were underestimated, the OH sink was overestimated, or significant unidentified sources exist. Anthropogenic activities (primarily biomass burning) contrib ute about half the net CH3Cl emitted from known sources. Anthropogenic emis sions account for only about 10% of the modeled CHCl3 sink. Although poorly constrained, significant fractions of tropospheric CH2Cl2 (25%), C2HCl3 (1 0%), and C2Cl4 (5%) are emitted from the surface ocean; the combined contri butions of C2Cl4 and C2HCl3 from all natural sources may be substantially h igher than the estimated oceanic flux.