Modelling the multiphase near-surface chemistry related to ozone depletions in polar spring

Piot, Matthias and von Glasow, Roland (2009) Modelling the multiphase near-surface chemistry related to ozone depletions in polar spring. Journal of Atmospheric Chemistry, 64 (2-3). pp. 77-105. ISSN 0167-7764

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Abstract

Near-total depletions of ozone have been observed in the Arctic spring since the mid1980s. The autocatalytic reaction cycles involving reactive halogens are now recognized to be of main importance for ozone depletion events in the polar boundary layer. We present sensitivity studies using the model MISTRA in the boxmodelmode on the influence of chemical species on these ozone depletion processes. In order to test the sensitivity of the chemistry under polar conditions, we compared base runs undergoing fluxes of either Br2,BrCl, or Cl2 to induce ozone depletions, with similar runs including a modification of thechemical conditions. The role of HCHO, H2O2, DMS, Cl2, C2H6, HONO, NO2, and RONO2 was investigated. Cases with elevated mixing ratios of HCHO, H2O2, DMS, Cl2, and HONO induceda shift in bromine speciation from Br/BrO to HOBr/HBr, while high mixing ratios of C2H6 induced a shift from HOBr/HBr to Br/BrO. The shifts from Br/BrO to HOBr/HBr accelerated the aerosol debromination, but also increased the total amount of deposited bromine at thesurface (mainly via increased deposition of HOBr). For all NOy species studied (HONO, NO2, RONO2) the chemistry is characterized by an increased bromine deposition on snow reducing the amount of reactive bromine in the air. Ozone is less depleted under conditions of high mixing ratios of NOx. The production of HNO3 led to the acid displacement of HCl, and the release of chlorine out of salt aerosol (Cl2 or BrCl) increased.

Item Type: Article
Faculty \ School: Faculty of Science > School of Environmental Sciences
Depositing User: Rosie Cullington
Date Deposited: 31 May 2011 14:19
Last Modified: 21 Apr 2020 17:43
URI: https://ueaeprints.uea.ac.uk/id/eprint/31594
DOI: 10.1007/s10874-010-9170-1

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