Abstract
Methane (CH4) emission reduction to limit warming to 1.5 °C can be tracked by analyzing CH4 concentration and its isotopic composition (δ13C, δD) simultaneously. Based on reconstructions of the temporal trends, latitudinal, and vertical gradient of CH4 and δ13C from 1985 to 2020 using an atmospheric chemistry transport model, we show (1) emission reductions from oil and gas exploitation (ONG) since the 1990s stabilized the atmospheric CH4 growth rate in the late 1990s and early 2000s, and (2) emissions from farmed animals, waste management, and coal mining contributed to the increase in CH4 since 2006. Our findings support neither the increasing ONG emissions reported by the EDGARv6 inventory during 1990–2020 nor the large unconventional emissions increase reported by the GAINSv4 inventory since 2006. Total fossil fuel emissions remained stable from 2000 to 2020, most likely because the decrease in ONG emissions in some regions offset the increase in coal mining emissions in China.
| Original language | English |
|---|---|
| Article number | 147 |
| Number of pages | 15 |
| Journal | Communications Earth and Environment |
| Volume | 5 |
| Issue number | 1 |
| DOIs | |
| Publication status | Published - 17 Apr 2024 |
Bibliographical note
Publisher Copyright:© The Author(s) 2024.
Funding
This work was made possible by the exceptional efforts of NOAA ESRL, CU-INSTAAR, Tohoku University (TU), and the National Institute of Polar Research (NIPR) in providing high-quality atmospheric measurements of CH4 and stable isotope compositions. We extend our gratitude to the Japanese Antarctic Research Expedition (JARE) Science Program staff and the Norwegian Polar Institute for their diligent collection of air samples in Syowa, Antarctica, and Ny-\u00C5lesund, Svalbard. Special thanks to Prof. Akihiko Ito for sharing wetland and rice emission data from the VISIT model, Dr. Sourish Basu for recommending the mass conservation test (Fig.\u00A0S5), and Dr. John Miller for highlighting KIE uncertainty issues at the TransCom-2022 meeting in Wageningen. Earth Simulator was used for simulation via the support of the Japan Agency for Marine-Earth Science and Technology. This research was supported by the Arctic Challenge for Sustainability II (ArCS-II) project (grant no. JPMXD1420318865), funded by Japan\u2019s Ministry of Education, Culture, Sports, Science and Technology (MEXT). This work was made possible by the exceptional efforts of NOAA ESRL, CU-INSTAAR, Tohoku University (TU), and the National Institute of Polar Research (NIPR) in providing high-quality atmospheric measurements of CH and stable isotope compositions. We extend our gratitude to the Japanese Antarctic Research Expedition (JARE) Science Program staff and the Norwegian Polar Institute for their diligent collection of air samples in Syowa, Antarctica, and Ny-\u00C5lesund, Svalbard. Special thanks to Prof. Akihiko Ito for sharing wetland and rice emission data from the VISIT model, Dr. Sourish Basu for recommending the mass conservation test (Fig. ), and Dr. John Miller for highlighting KIE uncertainty issues at the TransCom-2022 meeting in Wageningen. Earth Simulator was used for simulation via the support of the Japan Agency for Marine-Earth Science and Technology. This research was supported by the Arctic Challenge for Sustainability II (ArCS-II) project (grant no. JPMXD1420318865), funded by Japan\u2019s Ministry of Education, Culture, Sports, Science and Technology (MEXT). 4
| Funders | Funder number |
|---|---|
| CU-INSTAAR | |
| Tohoku University | |
| Norsk Polarinstitutt | |
| NOAA ESRL | |
| Ministry of Education, Culture, Sports, Science and Technology | |
| Japan Agency for Marine-Earth Science and Technology | JPMXD1420318865 |
| Japan Agency for Marine-Earth Science and Technology | |
| National Institute of Polar Research | JPMXD1420318865 |
| National Institute of Polar Research |
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