Modelling the Inorganic Bromine Partitioning in the Tropical Tropopause over the Pacific Ocean

MARÍA NAVARRO; ALFONSO SAIZ-LOPEZ; CARLOS A CUEVAS; RAFAEL P. FERNANDEZ; ELLIOT ATLAS; XAVIER RODRIGUEZ-LLOEVERAS; DOUGLAS E. KINNISON; JEAN-FRANCOISE LAMARQUE; SIMONE TILMES; TROY THORNBERRY; ANDREW ROLLINS; JAMES ELKINS; CARLOS FERRERO, JUAN; FREED MOORE

ATMOSPHERIC CHEMISTRY AND PHYSICS

COPERNICUS PUBLICATIONS

Lugar: Gottingen; Año: 2017 vol. 17 p. 9917 - 9930

1680-7316

The stratospheric inorganic bromine burden (Bry) arising from the degradation of brominated very short-lived organic substances (VSL org ), and its partitioning between reactive and reservoir species, is needed for a comprehensive assessment of the ozone depletion potential of brominated trace gases. Here we present modelled inorganic bromine abundances over the Pacific tropical tropopause based on aircraft observations of VSL org of two campaigns of the Airborne Tropical TRopopause EXperiment (ATTREX 2013 carried out over eastern Pacific and ATTREX 2014 carried out over the western Pacific) and chemistry-climate simulations (along ATTREX flight tracks) using the specific meteorology prevailing. Using the Community Atmosphere Model with Chemistry (CAM-Chem), we model that BrO and Br are the daytime dominant species. Integrated across all ATTREX flights BrO represents ~ 43 % and 48 % of daytime Bry abundance at 17 km over the Western and Eastern Pacific, respectively. The results also show zones where Br/BrO >1 depending on the solar zenith angle (SZA), ozone concentration and temperature. On the other hand, BrCl and BrONO 2 were found to be the dominant night-time species with ~ 61% and 56 % of abundance at 17 km over the Western and Eastern Pacific, respectively. The western-to-eastern differences in the partitioning of inorganic bromine are explained by different abundances of ozone (O3), nitrogen dioxide (NO2) , and total inorganic chlorine (Cly).