Hossaini, R, Chipperfield, MP orcid.org/0000-0002-6803-4149, Saiz-Lopez, A et al. (5 more authors) (2016) A global model of tropospheric chlorine chemistry: Organic versus inorganic sources and impact on methane oxidation. Journal of Geophysical Research: Atmospheres, 121 (23). 14,271-14,297. ISSN 2169-897X
Abstract
Chlorine atoms (Cl) are highly reactive toward hydrocarbons in the Earth's troposphere, including the greenhouse gas methane (CH₄). However, the regional and global CH₄ sink from Cl is poorly quantified as tropospheric Cl concentrations ([Cl]) are uncertain by ~2 orders of magnitude. Here we describe the addition of a detailed tropospheric chlorine scheme to the TOMCAT chemical transport model. The model includes several sources of tropospheric inorganic chlorine (Cly), including (i) the oxidation of chlorocarbons of natural (CH₃Cl, CHBr₂Cl, CH₂BrCl, and CHBrCl₂) and anthropogenic (CH₂Cl₂, CHCl₃, C₂Cl₄, C₂HCl₃, and CH₂ClCH₂Cl) origin and (ii) sea-salt aerosol dechlorination. Simulations were performed to quantify tropospheric [Cl], with a focus on the marine boundary layer, and quantify the global significance of Cl atom CH₄ oxidation. In agreement with observations, simulated surface levels of hydrogen chloride (HCl), the most abundant Cly reservoir, reach several parts per billion (ppb) over polluted coastal/continental regions, with sub-ppb levels typical in more remote regions. Modeled annual mean surface [Cl] exhibits large spatial variability with the largest levels, typically in the range of 1–5 × 104 atoms cm¯³, in the polluted northern hemisphere. Chlorocarbon oxidation provides a tropospheric Cly source of up to ~4320 Gg Cl/yr, sustaining a background surface [Cl] of <0.1 to 0.5 × 103 atoms cm¯³ over large areas. Globally, we estimate a tropospheric methane sink of ~12–13 Tg CH₄/yr due the CH₄ + Cl reaction (~2.5% of total CH₄ oxidation). Larger regional effects are predicted, with Cl accounting for ~10 to >20% of total boundary layer CH₄ oxidation in some locations.
Metadata
Item Type: | Article |
---|---|
Authors/Creators: |
|
Copyright, Publisher and Additional Information: | © 2016. The Authors. This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited. |
Keywords: | chlorine; Cl atoms; methane; VSLS; troposphere; sea salt |
Dates: |
|
Institution: | The University of Leeds |
Academic Units: | The University of Leeds > Faculty of Environment (Leeds) > School of Earth and Environment (Leeds) > Inst for Climate & Atmos Science (ICAS) (Leeds) The University of Leeds > Faculty of Environment (Leeds) > School of Earth and Environment (Leeds) > National Centre for Atmos Science (NCAS) (Leeds) |
Funding Information: | Funder Grant number NERC NE/J02449X/1 NERC no ext. ref. NERC No External Reference |
Depositing User: | Symplectic Publications |
Date Deposited: | 06 Feb 2017 13:59 |
Last Modified: | 23 Jun 2023 22:22 |
Published Version: | https://doi.org/10.1002/2016JD025756 |
Status: | Published |
Publisher: | American Geophysical Union |
Identification Number: | 10.1002/2016JD025756 |
Open Archives Initiative ID (OAI ID): | oai:eprints.whiterose.ac.uk:111829 |