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Vitenskapelig tidsskriftspublikasjon

Observations of 1,2-dichloroethane from the AGAGE and NOAA networks and derived global and regional emissions

Pitt, Joseph R.; Rust, Dominique; Ganesan, Anita; Western, Luke M.; Vollmer, Martin K.; Mühle, Jens; Bühlmann, Tobias; Harth, Christina M.; Montzka, Stephen A.; Hall, Brad D.; Vimont, Isaac J.; Manning, Alistair J.; Redington, Alison L.; Henne, Stephan; Melo, Daniela B.; Annadate, Saurabh; Constantin, Lionel; Murphy, Brendan M.; Rigby, Matthew; Young, Dickon; O'Doherty, Simon; Wenger, Angelina; Lunder, Chris René; Hermansen, Ove; Wagenhäuser, Thomas; Engel, Andreas; Arduini, Jgor; Maione, Michela; Yun, Jaegeun; Mitrevski, Blagoj; Krummel, Paul B.; Fraser, Paul J.; Kim, Jooil; Wang, Ray H. J.; Rhee, Tae Siek; Salameh, Peter K.; Spain, T. Gerard; Reimann, Stefan; Prinn, Ronald G.; Weiss, Ray F.; Stanley, Kieran M.

Publikasjonsdetaljer

Tidsskrift: Atmospheric Chemistry and Physics (ACP), vol. 26, 10167–10195, 21. juli 2026

Doi: doi.org/10.5194/acp-26-10167-2026
Arkiv: hdl.handle.net/11250/5538345
Arkiv: nva.sikt.no/registration/019face941d4-a1394aae-272e-45ef-ae1e-ad869c823e26

Sammendrag:
For the first time, we present long-term, ongoing atmospheric measurements of 1,2-dichloroethane (DCE, CH2ClCH2Cl) from the Advanced Global Atmospheric Gases Experiment (AGAGE) and National Oceanic and Atmospheric Administration (NOAA) global monitoring networks. DCE is an industrially produced, very short-lived chlorinated substance (Cl-VSLS) that has the potential to contribute chlorine to the stratosphere and cause ozone depletion. Compared to other Cl-VSLS, DCE is produced in higher volumes for its primary use as a feedstock in polyvinyl chloride (PVC) manufacture. This production has sustained annual mean mole fractions at the Earth's surface of between 5 and 10 ppt during 2017–2023, making it the third most abundant Cl-VSLS after dichloromethane and chloroform. In this study we estimate mean global emissions for 2017–2023 of 453 ± 185 Gg yr−1 using the AGAGE observations, and 525 ± 209 Gg yr−1 using the NOAA observations. We also use AGAGE measurements to estimate regional emissions for northwest Europe (2.06 [1.31, 2.65] Gg yr−1) and California (0.23 [0, 0.37] Gg yr−1), two domains with sufficient observational coverage to enable this approach. Our global emissions estimates are consistent (within uncertainties) with the only previously published estimate by Hossaini et al. (2024), whereas our regional emissions estimates are at least an order of magnitude smaller than those in that study. This suggests global total emissions may be well constrained, but their spatial distribution remains uncertain.