Articles | Volume 24, issue 2
https://doi.org/10.5194/acp-24-1415-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-24-1415-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Estimation of the atmospheric hydroxyl radical oxidative capacity using multiple hydrofluorocarbons (HFCs)
Climate and Environmental Research Institute NILU, 2007 Kjeller, Norway
Stephen A. Montzka
Global Monitoring Laboratory, NOAA, Boulder, CO 80305, USA
Martin K. Vollmer
Laboratory for Air Pollution and Environmental Technology, Empa, Swiss Federal Laboratories for Materials Science and Technology, 8600 Dübendorf, Switzerland
Jgor Arduini
Department of Pure and Applied Sciences, University of Urbino, Urbino, 61029, Italy
Molly Crotwell
Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO 80309, USA
Global Monitoring Laboratory, NOAA, Boulder, CO 80305, USA
Paul B. Krummel
CSIRO Environment, Aspendale, Victoria, 3195, Australia
Chris Lunder
Climate and Environmental Research Institute NILU, 2007 Kjeller, Norway
Jens Mühle
Scripps Institution of Oceanography, University of California San Diego, La Jolla, CA 92093, USA
Simon O'Doherty
School of Chemistry, University of Bristol, Bristol, BS8 1TS, UK
Ronald G. Prinn
Center for Global Change Science, Massachusetts Institute of Technology, Cambridge, MA 02139, USA
Stefan Reimann
Laboratory for Air Pollution and Environmental Technology, Empa, Swiss Federal Laboratories for Materials Science and Technology, 8600 Dübendorf, Switzerland
Isaac Vimont
Global Monitoring Laboratory, NOAA, Boulder, CO 80305, USA
Hsiang Wang
School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA 30332-0340, USA
Ray F. Weiss
Scripps Institution of Oceanography, University of California San Diego, La Jolla, CA 92093, USA
Dickon Young
School of Chemistry, University of Bristol, Bristol, BS8 1TS, UK
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Cited
3 citations as recorded by crossref.
- The impact of internal climate variability on OH trends between 2005 and 2014 Q. Zhu et al. 10.1088/1748-9326/ad4b47
- Human activities now fuel two-thirds of global methane emissions R. Jackson et al. 10.1088/1748-9326/ad6463
- A computational study on the kinetics of OH radical reactions with fluorinated dimethyl sulfides in the atmospheric window S. Sunitha & B. Rajakumar 10.1016/j.cplett.2024.141478
3 citations as recorded by crossref.
- The impact of internal climate variability on OH trends between 2005 and 2014 Q. Zhu et al. 10.1088/1748-9326/ad4b47
- Human activities now fuel two-thirds of global methane emissions R. Jackson et al. 10.1088/1748-9326/ad6463
- A computational study on the kinetics of OH radical reactions with fluorinated dimethyl sulfides in the atmospheric window S. Sunitha & B. Rajakumar 10.1016/j.cplett.2024.141478
Latest update: 23 Nov 2024
Short summary
The hydroxyl radical determines the atmospheric lifetimes of numerous species including methane. Since OH is very short-lived, it is not possible to directly measure its concentration on scales relevant for understanding its effect on other species. Here, OH is inferred by looking at changes in hydrofluorocarbons (HFCs). We find that OH levels have been fairly stable over our study period (2004 to 2021), suggesting that OH is not the main driver of the recent increase in atmospheric methane.
The hydroxyl radical determines the atmospheric lifetimes of numerous species including methane....
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