Atmos. Chem. Phys., 19, 1703–1719, 2019 https://doi.org/10.5194/acp-19-1703-2019 © Author(s) 2019. This work is distributed under the Creative Commons Attribution 4.0 License. Evidence for a major missing source in the global chloromethane budget from stable carbon isotopes Enno Bahlmann1,2, Frank Keppler3,4,5, Julian Wittmer6,7, Markus Greule3,4, Heinz Friedrich Schöler3, Richard Seifert1, and Cornelius Zetzsch5,6 1Institute of Geology, University Hamburg, Bundesstrasse 55, 20146 Hamburg, Germany 2Leibniz Centre for Tropical Marine Research, Fahrenheitstraße 6, 28359 Bremen, Germany 3Institute of Earth Sciences, Heidelberg University, Im Neuenheimer Feld 234–236, 69120 Heidelberg, Germany 4Heidelberg Center for the Environment (HCE), Heidelberg University, 69120 Heidelberg, Germany 5Max-Planck-Institute for Chemistry, Hahn-Meitner-Weg 1, 55128 Mainz, Germany 6Atmospheric Chemistry Research Unit, BayCEER, University of Bayreuth, Dr Hans-Frisch Strasse 1–3, 95448 Bayreuth, Germany 7Agilent Technologies Sales & Services GmbH & Co. KG, Hewlett-Packard-Str. 8, 76337 Waldbronn, Germany Correspondence: Enno Bahlmann (
[email protected]) Received: 17 August 2018 – Discussion started: 11 September 201 Revised: 17 January 2019 – Accepted: 18 January 2019 – Published: 8 February 2019 Abstract. Chloromethane (CH3Cl) is the most important with the OH-driven seasonal cycle in tropospheric mixing ra- natural input of reactive chlorine to the stratosphere, con- tios. tributing about 16 % to stratospheric ozone depletion. Due Applying these new values for the carbon isotope effect to the phase-out of anthropogenic emissions of chlorofluoro- to the global CH3Cl budget using a simple two hemispheric carbons, CH3Cl will largely control future levels of strato- box model, we derive a tropical rainforest CH3Cl source spheric chlorine.