Comparing the effect of Anthropogenically Amplified Halogen Natural Emissions on Tropospheric Ozone Chemistry between Pre‐Industrial and Present‐Day

BARRERA, JAVIER A.; KINNISON, DOUGLAS E.; FERNANDEZ, RAFAEL P.; LAMARQUE, JEAN?FRANÇOIS; CUEVAS, CARLOS A.; TILMES, SIMONE; SAIZ?LOPEZ, ALFONSO

Journal of Geophysical Research: Atmospheres

Wiley

Año: 2023

2169-897X

Reactive halogens (X+XO, X= I, Br or Cl) catalytically destroy a fraction of tropospheric ozone under present-day (PD) conditions, however, their distribution and potential impact on tropospheric ozone under pre-industrial (PI) conditions remain largely unexplored. This study uses the Community Atmospheric Model with Chemistry (CAM˗Chem) to investigate the effect of anthropogenically amplified natural emissions of halogenated species and their subsequent chemistry on tropospheric ozone under PI and PD atmospheric conditions. Model results show that the global tropospheric ozone depletion due to natural halogens is slightly more sensitive in PI than PD, with percentage changes in tropospheric ozone burden (TOB) of ˗14.1±0.6% for PI and ˗12.9±0.6% for PD. Individually, the role of iodine and chlorine in ozone depletion is equivalent in both periods (ΔTOBI: ∼ ˗7% and ΔTOBCl: ∼ ˗2.5%), while bromine plays a larger role in PI (ΔTOBBr: ˗5.5±0.6 %) vs. PD (ΔTOBBr: ˗4.3±0.7%). The increase in anthropogenic ozone precursor emissions from PI to PD has amplified the natural emission of inorganic halogens, as well as a shift in the partitioning of inorganic halogens from reactive to reservoir species. Consequently, halogen-driven ozone depletion from the surface to the free troposphere is larger in PI than PD. In contrast, in the upper troposphere, the ozone depletion is larger in PD influenced mainly by stratospheric intrusion of long-lived reactive halogens. This study highlights the importance of including a complete chemical coupling of natural halogens and atmospheric pollutants in chemistry-climate models to adequately assess their effects on tropospheric ozone in a changing climate