Articles | Volume 20, issue 14
https://doi.org/10.5194/acp-20-8405-2020
https://doi.org/10.5194/acp-20-8405-2020
Research article
 | 
17 Jul 2020
Research article |  | 17 Jul 2020

Strong sensitivity of the isotopic composition of methane to the plausible range of tropospheric chlorine

Sarah A. Strode, James S. Wang, Michael Manyin, Bryan Duncan, Ryan Hossaini, Christoph A. Keller, Sylvia E. Michel, and James W. C. White

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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Sarah Strode on behalf of the Authors (24 Apr 2020)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (08 May 2020) by Patrick Jöckel
RR by Anonymous Referee #2 (22 May 2020)
RR by Anonymous Referee #1 (29 May 2020)
ED: Publish subject to minor revisions (review by editor) (29 May 2020) by Patrick Jöckel
AR by Sarah Strode on behalf of the Authors (05 Jun 2020)  Author's response    Manuscript
ED: Publish as is (19 Jun 2020) by Patrick Jöckel
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Short summary
The 13C : 12C isotopic ratio in methane (CH4) provides information about CH4 sources, but loss of CH4 by reaction with OH and chlorine (Cl) also affects this ratio. Tropospheric Cl provides a small and uncertain sink for CH4 but has a large effect on its isotopic ratio. We use the GEOS model with several different Cl fields to test the sensitivity of methane's isotopic composition to tropospheric Cl. Cl affects the global mean, hemispheric gradient, and seasonal cycle of the isotopic ratio.
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