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):
- Global annual average 𝛿D-CH4, global annual average uncertainty, trend, and trend uncertainty since 2005: ch3d_glob_mean_unc.xlsx
- Global annual average 𝛿13C-CH4, global annual average uncertainty, trend, and trend uncertainty since 1999: ch4c13_glob_mean_unc.xlsx
𝛿D-CH4 site data files:
- INSTAAR Stable Isotope Laboratory Data:
- Folder name: INSTAAR_ch3d
- The folder contains atmospheric 𝛿D-CH4 measurements from the following sampling sites:
- Alert, Canada (ALT): alt.ch4h2.txt
- Barrow Atmospheric Baseline Observatory, Alaska, USA (BRW): brw.ch4h2.txt
- Cold Bay, Alaska, USA (CBA): cba.ch4h2.txt
- Cape Grim, Tasmania, Australia (CGO): cgo.ch4h2.txt
- Cape Kumukahi, Hawaii, USA (KUM): kum.ch4h2.txt
- Mace Head, Ireland (MHD): mhd.ch4h2.txt
- Tutuila, American Samoa (SMO): smo.ch4h2.txt
- South Pole, Antarctica (SPO): spo.ch4h2.txt
- Ny-Alesund, Svalbard, Norway (ZEP): zep. ch4h2.txt
- Dataset Contact: Sylvia Michel: michel@colorado.edu
- Max Planck Institute for Biogeochemistry (MPI-BGC) Data:
- Folder name: MPI-BGC_ch3d
- The folder contains atmospheric 𝛿D-CH4 measurements from the following sampling sites:
- Alert, Canada (ALT): Flasks_ALT_dH2(CH4)_v2025.1.txt
- Cape Verde Atmospheric Observatory, Cape Verde (CVO): Flasks_CVO_dH2(CH4)_v2025.1.txt
- Neumayer Station, Antarctica (GVN/NMY): Flasks_GVN_dH2(CH4)_v2025.1.txt
- Gobabeb Station, Namibia (NMB): Flasks_NMB_dH2(CH4)_v2025.1.txt
- Shetland Islands, United Kingdom (SIS): Flasks_SIS_dH2(CH4)_v2025.1.txt
- Villium Research Station, Greenland (VRS/SNO): Flasks_SNO_dH2(CH4)_v2025.1.txt
- Zotina Tall Tower Observatory, Siberia, Russia (ZOT): Flasks_ZOT_dH2(CH4)_v2025.1.txt
- Public repository link: https://www.edmond.mpg.de/dataset.xhtml?persistentId=doi:10.17617/3.V2EXHD
- Dataset contact: Dr. Heiko Moossen (moossen@bgc-jena.mpg.de)
- Utrecht University’s Institute for Marine and Atmospheric Research (UU/IMAU) Data:
- Folder name: UU-IMAU_ch3d
- The folder contains atmospheric 𝛿D-CH4 measurements from the following sampling sites:
- Neumayer Station, Antarctica (GVN):
- Ny-Alesund, Svalbard, Norway (ZEP):
- Dataset contact: Dr. Thomas Röckmann (rockmann@uu.nl)
- Tohoku University and the National Institute for Polar Research (TU/NIPR) Data:
- Folder name: TU-NIPR_ch3d
- The folder contains atmospheric 𝛿D-CH4 measurements from the following sampling sites:
- Nyvolesund Station, Norway (NYA):
- Syowa Station, Antarctica (SYO): ch3d_syo_TU-NIPR.txt
- Dataset contact: Dr. Shinji Morimoto: (mon@tohoku.ac.jp)
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.
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