Abstract
Monitoring the spatial distribution and trends in surface greenhouse gas (GHG) fluxes, as well as flux attribution to natural and anthropogenic processes, is essential to track progress under the Paris Agreement and to inform its global stocktake. This study updates earlier syntheses (Petrescu et al., 2020, 2021, 2023), provides a consolidated synthesis of CH4 emissions using bottom-up (BU) and top-down (TD) approaches for the European Union (EU), and is expanded to include seven additional countries with large anthropogenic and/or natural emissions (the USA, Brazil, China, India, Indonesia, Russia, and the Democratic Republic of the Congo (DR Congo)). Our aim is to demonstrate the use of different emission estimates to help improve national GHG emission inventories for a diverse geographical range of stakeholders. We use updated national GHG inventories (NGHGIs) reported by Annex I parties under the United Nations Framework Convention on Climate Change (UNFCCC) in 2023 and the latest available biennial update reports (BURs) reported by non-Annex I parties. Comparing NGHGIs with other approaches highlights that different system boundaries are a key source of divergence. A key system boundary difference is whether anthropogenic and natural fluxes are included and, if they are, how fluxes belonging to these two sources are partitioned. Over the studied period, the total CH4 emission estimates in the EU, the USA, and Russia show a steady decreasing trend since 1990, while for the non-Annex I emitters analyzed in this study, Brazil, China, India, Indonesia, and DR Congo, CH4 emissions have generally increased. Quantitatively, in the EU the mean of 2015-2020 anthropogenic UNFCCC NGHGIs (15±1.8 Tg CH4 yr-1) and the mean of the BU CH4 emissions (17.8 (16-19) Tg CH4 yr-1) generally agree on the magnitude, while inversions show higher emission estimates (medians of 21 (19-22) Tg CH4 yr-1 and 24 (22-25) Tg CH4 yr-1 for the three regional and six global inversions, respectively), as they include natural emissions, which for the EU were quantified at 6.6 Tg CH4 yr-1 (Petrescu et al., 2023). Similarly, for the other Annex I parties in this study (the USA and Russia), the gap between the BU anthropogenic and total TD emissions is partly explained by the natural emissions. For the non-Annex I parties, anthropogenic CH4 estimates from UNFCCC BURs show large differences compared to the other global-inventory-based estimates and even more compared to atmospheric ones. This poses an important potential challenge to monitoring the progress of the global CH4 pledge and the global stocktake. Our analysis provides a useful baseline to prepare for the influx of inventories from non-Annex I parties as regular reporting starts under the enhanced transparency framework of the Paris Agreement. By systematically comparing the BU and TD methods, this study provides recommendations for more robust comparisons of available data sources and hopes to steadily engage more parties in using observational methods to complement their UNFCCC inventories, as well as considering their natural emissions. With anticipated improvements in atmospheric modeling and observations, as well as modeling of natural fluxes, future development needs to resolve knowledge gaps in the BU and TD approaches and to better quantify the remaining uncertainty. TD methods may emerge as a powerful tool to help improve NGHGIs of CH4 emissions, but further confidence is needed in the comparability and robustness of the estimates. The referenced datasets related to figures are available at 10.5281/zenodo.12818506 (Petrescu et al., 2024).
Original language | English |
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Pages (from-to) | 4325-4350 |
Number of pages | 26 |
Journal | Earth System Science Data |
Volume | 16 |
Issue number | 9 |
Early online date | 25 Sept 2024 |
DOIs | |
Publication status | Published - 2024 |
Bibliographical note
Publisher Copyright:© Copyright: 2024 Ana Maria Roxana Petrescu et al.
Funding
The lead author would like to thank former colleagues, Chunjing Qiu and Matthew McGrath, for previous work done for the EU-funded VERIFY project. FAOSTAT statistics are produced and disseminated with the support of its member countries to the FAO regular budget. We acknowledge the work of current and former members of the EDGAR group (Marilena Muntean, Diego Guizzardi, Monica Crippa, Edwin Schaaf, Efisio Solazzo, Gabriel David Orreggioni, and Jos Olivier). Claire Granier, Sekou Keito, and Antonin Soulie from Laboratoire d Aerologie, CNRS, Toulouse, France, are acknowledged for their work and support in the construction of the TNO-CoCO2-PED18-21. This research has been supported by the European Commission s Horizon 2020 Framework Programme (CoCO2, grant no. 958927). Part of Glen P. Peters work was supported by the European Union s Horizon Europe Research and Innovation program (grant no. 101081395 (EYE-CLIMA)). Development of MIROC4-ACTM is supported by the Environment Research and Technology Development Fund (grant no. JP-MEERF21S20800) and the Arctic Challenge for Sustainability phase II (ArCS-II; grant no. JPMXD1420318865) project. Dominik Brunner was supported by FORMAS (grant no. 2018-01794), the European Union (H2020, grant no. 101015825; TRIAGE), and the Swedish Research Council (VR; grant no. 2022-03841). Pierre Regnier received funding from the European Union s Horizon 2020 Research and Innovation program (grant no. 101003536 (ESM2025-Earth System Models for the Future)) and from the FRS-FRNS PDR project T.0191.23 CH4- lakes. Annual, gap-filled, and harmonized NGHGI uncertainty estimates for the EU were provided by the EU GHG inventory team (European Environment Agency and its European Topic Centre on Climate Change Mitigation). Ronny Lauerwald received funding from French state aid, managed by ANR under the Investissements d Avenir program (ANR-16-CONV-0003).Wenxin Zhang was supported by grants from the Swedish Research Council (2020-05338) and Swedish National Space Agency (grant no. 209/19). Part of John R. Worden s work was carried out at the Jet Propulsion Laboratory, California Institute of Technology, under contract with the National Aeronautics and Space Administration (NASA). Part of Philippe Peylin s work was supported by the European Commission H2020 Framework Programme (grant no. 776810 (VERIFY)). Part of Stijn N. C. Dellaert s and Hugo Denier van der Gon s work was also supported by European Union s Horizon Europe Research and Innovation program (grant no. 101081322 (AVENGERS)). This research has been supported by the European Commission's Horizon 2020 Framework Programme (CoCO, grant no. 958927). Part of Glen P. Peters' work was supported by the European Union's Horizon Europe Research and Innovation program (grant no. 101081395 (EYE-CLIMA)). Development of MIROC4-ACTM is supported by the Environment Research and Technology Development Fund (grant no. JP-MEERF21S20800) and the Arctic Challenge for Sustainability phase II (ArCS-II; grant no. JP-MXD1420318865) project. Dominik Brunner was supported by FORMAS (grant no. 2018-01794), the European Union (H2020, grant no. 101015825; TRIAGE), and the Swedish Research Council (VR; grant no. 2022-03841). Pierre Regnier received funding from the European Union's Horizon 2020 Research and Innovation program (grant no. 101003536 (ESM2025 \u2013 Earth System Models for the Future)) and from the FRS-FRNS PDR project T.0191.23 CH-lakes. Annual, gap-filled, and harmonized NGHGI uncertainty estimates for the EU were provided by the EU GHG inventory team (European Environment Agency and its European Topic Centre on Climate Change Mitigation). Ronny Lauerwald received funding from French state aid, managed by ANR under the Investissements d'Avenir program (ANR-16-CONV-0003). Wenxin Zhang was supported by grants from the Swedish Research Council (2020-05338) and Swedish National Space Agency (grant no. 209/19). Part of John R. Worden's work was carried out at the Jet Propulsion Laboratory, California Institute of Technology, under contract with the National Aeronautics and Space Administration (NASA). Part of Philippe Peylin's work was supported by the European Commission H2020 Framework Programme (grant no. 776810 (VERIFY)). Part of Stijn N. C. Dellaert's and Hugo Denier van der Gon's work was also supported by European Union's Horizon Europe Research and Innovation program (grant no. 101081322 (AVENGERS)).
Funders | Funder number |
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European Commission s Horizon 2020 Framework Programme | |
National Aeronautics and Space Administration | |
European Commission's Horizon 2020 framework programme | |
European Commission | |
Laboratoire d Aerologie | |
European Union s Horizon Europe Research and Innovation program | |
Hugo Denier | |
European Environment Agency | |
European Union's Horizon Europe Research and Innovation program | 101081395 |
CoCO | 958927 |
Environment Research and Technology Development Fund | JP-MEERF21S20800 |
European Union s Horizon 2020 Research and Innovation program | 101003536 |
Svenska Forskningsrådet Formas | 2018-01794 |
Horizon 2020 | ESM2025, 101003536 |
Horizon 2020 Framework Programme | 101015825 |
Agence Nationale de la Recherche | ANR-16-CONV-0003, 2020-05338 |
European Commission H2020 Framework Programme | 776810, 101081322 |
Arctic Challenge for Sustainability | JP-MXD1420318865 |
Vetenskapsrådet | 2022-03841 |
Centre National de la Recherche Scientifique | TNO-CoCO2-PED18-21 |
Swedish National Space Agency | 209/19 |