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Journal Articles (Data Paper) Earth System Science Data Year : 2023

The consolidated European synthesis of CO 2 emissions and removals for the European Union and United Kingdom: 1990–2020

Matthew Mcgrath
Ana Maria Roxana Petrescu
  • Function : Author
Philippe Peylin
  • Function : Author
Robbie Andrew
Bradley Matthews
Frank Dentener
Juraj Balkovič
  • Function : Author
Vladislav Bastrikov
  • Function : Author
Meike Becker
Gregoire Broquet
  • Function : Author
Audrey Fortems-Cheiney
  • Function : Author
Raphael Ganzenmüller
Giacomo Grassi
  • Function : Author
Ian Harris
  • Function : Author
Matthew Jones
  • Function : Author
Jürgen Knauer
Matthias Kuhnert
  • Function : Author
Guillaume Monteil
Saqr Munassar
Paul Palmer
Glen Peters
Chunjing Qiu
  • Function : Author
Mart-Jan Schelhaas
  • Function : Author
Oksana Tarasova
  • Function : Author
Matteo Vizzarri
Karina Winkler
Gianpaolo Balsamo
Antoine Berchet
Peter Briggs
  • Function : Author
Patrick Brockmann
  • Function : Author
Frédéric Chevallier
Giulia Conchedda
  • Function : Author
Monica Crippa
  • Function : Author
Stijn Dellaert
Hugo Denier van der Gon
Sara Filipek
  • Function : Author
Richard Fuchs
  • Function : Author
Michael Gauss
  • Function : Author
Christoph Gerbig
Diego Guizzardi
  • Function : Author
Dirk Günther
  • Function : Author
Richard Houghton
Greet Janssens-Maenhout
Bas Lerink
Ingrid Luijkx
Géraud Moulas
  • Function : Author
Marilena Muntean
  • Function : Author
Gert-Jan Nabuurs
  • Function : Author
Aurélie Paquirissamy
  • Function : Author
Lucia Perugini
Wouter Peters
Roberto Pilli
  • Function : Author
Julia Pongratz
Pierre Regnier
  • Function : Author
Marko Scholze
Yusuf Serengil
  • Function : Author
Pete Smith
Efisio Solazzo
Rona Thompson
Francesco Tubiello
Timo Vesala
  • Function : Author
Sophia Walther

Abstract

Quantification of land surface–atmosphere fluxes of carbon dioxide (CO2) and their trends and uncertainties is essential for monitoring progress of the EU27+UK bloc as it strives to meet ambitious targets determined by both international agreements and internal regulation. This study provides a consolidated synthesis of fossil sources (CO2 fossil) and natural (including formally managed ecosystems) sources and sinks over land (CO2 land) using bottom-up (BU) and top-down (TD) approaches for the European Union and United Kingdom (EU27+UK), updating earlier syntheses (Petrescu et al., 2020, 2021). Given the wide scope of the work and the variety of approaches involved, this study aims to answer essential questions identified in the previous syntheses and understand the differences between datasets, particularly for poorly characterized fluxes from managed and unmanaged ecosystems. The work integrates updated emission inventory data, process-based model results, data-driven categorical model results, and inverse modeling estimates, extending the previous period 1990–2018 to the year 2020 to the extent possible. BU and TD products are compared with the European national greenhouse gas inventory (NGHGI) reported by parties including the year 2019 under the United Nations Framework Convention on Climate Change (UNFCCC). The uncertainties of the EU27+UK NGHGI were evaluated using the standard deviation reported by the EU member states following the guidelines of the Intergovernmental Panel on Climate Change (IPCC) and harmonized by gap-filling procedures. Variation in estimates produced with other methods, such as atmospheric inversion models (TD) or spatially disaggregated inventory datasets (BU), originate from within-model uncertainty related to parameterization as well as structural differences between models. By comparing the NGHGI with other approaches, key sources of differences between estimates arise primarily in activities. System boundaries and emission categories create differences in CO2 fossil datasets, while different land use definitions for reporting emissions from land use, land use change, and forestry (LULUCF) activities result in differences for CO2 land. The latter has important consequences for atmospheric inversions, leading to inversions reporting stronger sinks in vegetation and soils than are reported by the NGHGI. For CO2 fossil emissions, after harmonizing estimates based on common activities and selecting the most recent year available for all datasets, the UNFCCC NGHGI for the EU27+UK accounts for 926 ± 13 Tg C yr−1, while eight other BU sources report a mean value of 948 [937,961] Tg C yr−1 (25th, 75th percentiles). The sole top-down inversion of fossil emissions currently available accounts for 875 Tg C in this same year, a value outside the uncertainty of both the NGHGI and bottom-up ensemble estimates and for which uncertainty estimates are not currently available. For the net CO2 land fluxes, during the most recent 5-year period including the NGHGI estimates, the NGHGI accounted for −91 ± 32 Tg C yr−1, while six other BU approaches reported a mean sink of −62 [-117,-49] Tg C yr−1, and a 15-member ensemble of dynamic global vegetation models (DGVMs) reported −69 [-152,-5] Tg C yr−1. The 5-year mean of three TD regional ensembles combined with one non-ensemble inversion of −73 Tg C yr−1 has a slightly smaller spread (0th–100th percentiles of [-135,+45] Tg C yr−1), and it was calculated after removing net land–atmosphere CO2 fluxes caused by lateral transport of carbon (crop trade, wood trade, river transport, and net uptake from inland water bodies), resulting in increased agreement with the NGHGI and bottom-up approaches. Results at the category level (Forest Land, Cropland, Grassland) generally show good agreement between the NGHGI and category-specific models, but results for DGVMs are mixed. Overall, for both CO2 fossil and net CO2 land fluxes, we find that current independent approaches are consistent with the NGHGI at the scale of the EU27+UK. We conclude that CO2 emissions from fossil sources have decreased over the past 30 years in the EU27+UK, while land fluxes are relatively stable: positive or negative trends larger (smaller) than 0.07 (−0.61) Tg C yr−2 can be ruled out for the NGHGI. In addition, a gap on the order of 1000 Tg C yr−1 between CO2 fossil emissions and net CO2 uptake by the land exists regardless of the type of approach (NGHGI, TD, BU), falling well outside all available estimates of uncertainties. However, uncertainties in top-down approaches to estimate CO2 fossil emissions remain uncharacterized and are likely substantial, in addition to known uncertainties in top-down estimates of the land fluxes. The data used to plot the figures are available at https://doi.org/10.5281/zenodo.8148461 (McGrath et al., 2023).

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Global Changes
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hal-04528076 , version 1 (02-04-2024)

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Matthew Mcgrath, Ana Maria Roxana Petrescu, Philippe Peylin, Robbie Andrew, Bradley Matthews, et al.. The consolidated European synthesis of CO 2 emissions and removals for the European Union and United Kingdom: 1990–2020. Earth System Science Data, 2023, 15 (10), pp.4295-4370. ⟨10.5194/essd-15-4295-2023⟩. ⟨hal-04528076⟩
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