Atmospheric data analyzed in “Microbial driver of 2006 – 2023 CH4 growth indicated by trends in atmospheric 𝛿D-CH4 and 𝛿13C-CH4”, PNAS

Atmospheric data analyzed in “Microbial driver of 2006 – 2023 CH4 growth indicated by trends in atmospheric 𝛿D-CH4 and 𝛿13C-CH4”, PNAS

Ben Riddell-Young1,2; Sylvia Englund Michel3,4; Xin Lan1,2; Pieter Tans3; Thomas Röckmann5; Bibhasvata Dasgupta5; Youmi Oh1,2; Lori Bruhwiler1,2; Ryo Fujita6; Taku Umezawa7,8; Shinji Morimoto7; John Miller2

1 Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, CO, 80309, USA

2 Global Monitoring Laboratory, National Oceanic and Atmospheric Administration, Boulder, CO, 80205, USA

3 Institute of Arctic and Alpine Research, University of Colorado, Boulder, CO, 80303, USA

4 Department of Atmospheric and Oceanic Sciences, University of Colorado, Boulder, CO, 80303, USA

5 Institute for Marine and Atmospheric research Utrecht, Utrecht University, The Netherlands

6 Meteorological Research Institute, Japan Meteorological Agency, Tsukuba, Japan

7 Tohoku University, Sendai, Japan

8 National Institute for Environmental Studies, Tsukuba, Japan

Corresponding Author: Ben Riddell-Young

E: ben.riddell-young@colorado.edu

Abstract:

This paper investigates the global annual average record of atmospheric methane (CH4) and the stable isotopic composition of atmospheric CH4 (𝛿D-CH4 and 𝛿13C-CH4). Atmospheric CH4 and 𝛿13C-CH4 global means are determined from the NOAA Global Monitoring Laboratories Global Greenhouse Gas Reference Network. Discrete data and descriptions of sampling methods are available on the NOAA GML website.

The 2005 to 2023 global mean atmospheric 𝛿D-CH4 was determined using a compilation of discrete measurements from several different laboratories at sampling sites around the world (see below). The data are presented on their original laboratory-specific calibration scales and are from sites that receive well-mixed air that is minimally influenced by local source, which are known as marine boundary layer reference sites. In the paper, the data were harmonized to the MPI-BGC scale using established laboratory offsets from Umezawa et al., 2018 (https://doi.org/10.5194/amt-11-1207-2018) and a recent intercomparison between INSTAAR and MPI-BGC. Alternatively, the data can be harmonized using a more recent estimate of laboratory offsets from Dasgupta et al., 2025 (https://doi.org/10.5194/egusphere-2025-2439), which differs slightly. Refer to Table S1 in the paper for offset values and uncertainties used.

All atmospheric data included in the paper are available here. If you would like to use the δD-CH4 data in publication, please contact benjamin.riddell-young@noaa.gov. If you would like to use the δ13C-CH4 data in publication, please contact sylvia.michel@colorado.edu. If you would like to use the CH4 data in publication, please also contact xin.lan@noaa.gov. If you would like to use the isotopic data from MPI, NIWA, or TU/NIPR in publications, please contact the data providers listed next to the data below.

Globally averaged data files (Figure 1 in manuscript):

𝛿D-CH4 site data files:

Fair Use Statement

These data are made freely available to the public and the scientific community in the belief that their wide dissemination will lead to greater understanding and new scientific insights. To ensure that GML receives fair credit for their work please include relevant citation text in publications. We encourage users to contact the data providers, who can provide detailed information about the measurements and scientific insight. In cases where the data are central to a publication, co-authorship for data providers may be appropriate.

Citation

Riddell-Young, B., Michel, S. E., Lan, X., Tans, P., Röckmann, T., Dasgupta, B., Oh, Y., Bruhwiler, L., Fujita, R., Umezawa, T., Morimoto, S., Miller, J. “Microbial driver of 2006 – 2023 CH4 growth indicated by trends in atmospheric 𝛿D-CH4 and 𝛿13C-CH4” PNAS. DOI: https://doi.org/10.1073/pnas.2516543122


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