- Western, Luke;
- Redington, Alison;
- Manning, Alistair;
- Trudinger, Cathy;
- Hu, Lei;
- Henne, Stephan;
- Fang, Xuekun;
- Kuijpers, Lambert;
- Theodoridi, Christina;
- Godwin, David;
- Arduini, Jgor;
- Dunse, Bronwyn;
- Engel, Andreas;
- Fraser, Paul;
- Harth, Christina;
- Krummel, Paul;
- Maione, Michela;
- Mühle, Jens;
- ODoherty, Simon;
- Park, Hyeri;
- Park, Sunyoung;
- Reimann, Stefan;
- Salameh, Peter;
- Say, Daniel;
- Schmidt, Roland;
- Schuck, Tanja;
- Siso, Carolina;
- Stanley, Kieran;
- Vimont, Isaac;
- Vollmer, Martin;
- Young, Dickon;
- Prinn, Ronald;
- Weiss, Ray;
- Montzka, Stephen;
- Rigby, Matthew
Global emissions of the ozone-depleting gas HCFC-141b (1,1-dichloro-1-fluoroethane, CH3CCl2F) derived from measurements of atmospheric mole fractions increased between 2017 and 2021 despite a fall in reported production and consumption of HCFC-141b for dispersive uses. HCFC-141b is a controlled substance under the Montreal Protocol, and its phase-out is currently underway, after a peak in reported consumption and production in developing (Article 5) countries in 2013. If reported production and consumption are correct, our study suggests that the 2017-2021 rise is due to an increase in emissions from the bank when appliances containing HCFC-141b reach the end of their life, or from production of HCFC-141b not reported for dispersive uses. Regional emissions have been estimated between 2017-2020 for all regions where measurements have sufficient sensitivity to emissions. This includes the regions of northwestern Europe, east Asia, the United States and Australia, where emissions decreased by a total of 2.3 ± 4.6 Ggyr-1, compared to a mean global increase of 3.0 ± 1.2 Ggyr-1 over the same period. Collectively these regions only account for around 30% of global emissions in 2020. We are not able to pinpoint the source regions or specific activities responsible for the recent global emission rise.