Recent Decreases in the Growth Rate of Atmospheric HCFC-22 Column Derived From the Ground-Based FTIR Harmonized Retrievals at 16 NDACC Sites

  • Minqiang Zhou
  • , Bavo Langerock
  • , Corinne Vigouroux
  • , Dan Smale
  • , Geoff Toon
  • , Alexander Polyakov
  • , James W. Hannigan
  • , Johan Mellqvist
  • , John Robinson
  • , Justus Notholt
  • , Kimberly Strong
  • , Emmanuel Mahieu
  • , Mathias Palm
  • , Maxime Prignon
  • , Nicolas Jones
  • , Omaira García
  • , Isamu Morino
  • , Isao Murata
  • , Ivan Ortega
  • , Tomoo Nagahama
  • Tyler Wizenberg, Victoria Flood, Kaley Walker, Martine De Mazière

Research output: Contribution to journalArticlepeer-review

2 Scopus citations

Abstract

HCFC-22 is an ozone-depleting substance with a greenhouse effect. The atmospheric mole fractions of HCFC-22 have been increasing since the 1950s. Within the NDACC-IRWG network, HCFC-22 mol fractions can be retrieved from solar absorption spectra measured by ground-based FTIR. However, only a few sites have provided HCFC-22 data sets. Here, we demonstrate a harmonized FTIR HCFC-22 retrieval strategy and generate a new global NDACC-IRWG HCFC-22 data set at 16 FTIR sites. The systematic and random uncertainties are 5.3%–8.7% and 3.2%–8.0%, respectively. A maximum HCFC-22 column annual growth rate was observed in 2009 with a mean of 7.65 ± 1.39 ppt/year, and the HCFC-22 annual growth rate decreased to 3.57 ± 1.39 ppt/year (2016–2020) and 2.15 ± 2.09 ppt/year (2021–2023). The annual growth rates derived from the FTIR measurements are compared to the ones derived from NOAA surface flask samplings and ACE-FTS satellite measurements, and the three independent data sets show a good agreement.

Original languageEnglish
Article numbere2024GL112470
JournalGeophysical Research Letters
Volume51
Issue number22
DOIs
StatePublished - Nov 28 2024
Externally publishedYes

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