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  5. The consolidated European synthesis of CH4 and N2O emissions for the European Union and United Kingdom: 1990–2019
 
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The consolidated European synthesis of CH4 and N2O emissions for the European Union and United Kingdom: 1990–2019

Author(s)
Petrescu, Ana Maria Roxana
Qiu, Chunjing
McGrath, Matthew J  
Peylin, Philippe  
Peters, Glen P.  
Ciais, Philippe  
Thompson, Rona L  
Tsuruta, Aki  
Brunner, Dominik  
Kuhnert, Matthias  
Matthews, Bradley  
Palmer, Paul I  
Tarasova, Oksana  
Regnier, Pierre  
Lauerwald, Ronny  
Bastviken, David  
Höglund-Isaksson, Lena  
Winiwarter, Wilfried  
Etiope, Giuseppe  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia  
Aalto, Tuula  
Balsamo, Gianpaolo  
Bastrikov, Vladislav  
Berchet, Antoine  
Brockmann, Patrick  
Ciotoli, Giancarlo  
Conchedda, Giulia  
Crippa, Monica  
Dentener, Frank  
Groot Zwaaftink, Christine  
Guizzardi, Diego  
Günther, Dirk  
Haussaire, Jean-Matthieu  
Houweling, Sander  
Janssens-Maenhout, Greet  
Kouyate, Massaer  
Leip, Adrian  
Leppänen, Antti  
Lugato, Emanuele  
Maisonnier, Manon  
Manning, Alistair J  
Markkanen, Tiina  
McNorton, Joe  
Muntean, Marilena  
Oreggioni, Gabriel  
Patra, Prabir K  
Perugini, Lucia  
Pison, Isabelle  
Raivonen, Maarit  
Saunois, Marielle  
Segers, Arjo  
Smith, Pete  
Solazzo, Efisio  
Tian, Hanqin  
Tubiello, Francesco N.  
Vesala, Timo  
van der Werf, Guido R  
Wilson, Chris  
Zaehle, Sönke  
Language
English
Obiettivo Specifico
OSA2: Evoluzione climatica: effetti e loro mitigazione
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Journal
Earth System Science Data  
Issue/vol(year)
/15 (2023)
ISSN
1866-3591
Publisher
Egu-Copernicus
Pages (printed)
1197–1268
Date Issued
2023
DOI
10.5194/essd-15-1197-2023
URI
https://www.earth-prints.org/handle/2122/16675
Abstract
Knowledge of the spatial distribution of the fluxes of greenhouse gases (GHGs) and their temporal variability as well as flux attribution to natural and anthropogenic processes is essential to monitoring the progress in mitigating anthropogenic emissions under the Paris Agreement and to inform its global stocktake. This study provides a consolidated synthesis of CH4 and N2O emissions using bottom-up (BU) and top-down (TD) approaches for the European Union and UK (EU27 + UK) and updates earlier syntheses (Petrescu et al., 2020, 2021). The work integrates updated emission inventory data, process-based model results, data-driven sector model results and inverse modeling estimates, and it extends the previous period of 1990–2017 to 2019. BU and TD products are compared with European national greenhouse gas inventories (NGHGIs) reported by parties under the United Nations Framework Convention on Climate Change (UNFCCC) in 2021. Uncertainties in NGHGIs, as reported to the UNFCCC by the EU and its member states, are also included in the synthesis. Variations in estimates produced with other methods, such as atmospheric inversion models (TD) or spatially disaggregated inventory datasets (BU), arise from diverse sources including within-model uncertainty related to parameterization as well as structural differences between models. By comparing NGHGIs with other approaches, the activities included are a key source of bias between estimates, e.g., anthropogenic and natural fluxes, which in atmospheric inversions are sensitive to the prior geospatial distribution of emissions. For CH4 emissions, over the updated 2015–2019 period, which covers a sufficiently robust number of overlapping estimates, and most importantly the NGHGIs, the anthropogenic BU approaches are directly comparable, accounting for mean emissions of 20.5 Tg CH4 yr−1 (EDGARv6.0, last year 2018) and 18.4 Tg CH4 yr−1 (GAINS, last year 2015), close to the NGHGI estimates of 17.5±2.1 Tg CH4 yr−1. TD inversion estimates give higher emission estimates, as they also detect natural emissions. Over the same period, high-resolution regional TD inversions report a mean emission of 34 Tg CH4 yr−1. Coarser-resolution global-scale TD inversions result in emission estimates of 23 and 24 Tg CH4 yr−1 inferred from GOSAT and surface (SURF) network atmospheric measurements, respectively. The magnitude of natural peatland and mineral soil emissions from the JSBACH–HIMMELI model, natural rivers, lake and reservoir emissions, geological sources, and biomass burning together could account for the gap between NGHGI and inversions and account for 8 Tg CH4 yr−1. For N2O emissions, over the 2015–2019 period, both BU products (EDGARv6.0 and GAINS) report a mean value of anthropogenic emissions of 0.9 Tg N2O yr−1, close to the NGHGI data (0.8±55 % Tg N2O yr−1). Over the same period, the mean of TD global and regional inversions was 1.4 Tg N2O yr−1 (excluding TOMCAT, which reported no data). The TD and BU comparison method defined in this study can be operationalized for future annual updates for the calculation of CH4 and N2O budgets at the national and EU27 + UK scales. Future comparability will be enhanced with further steps involving analysis at finer temporal resolutions and estimation of emissions over intra-annual timescales, which is of great importance for CH4 and N2O, and may help identify sector contributions to divergence between prior and posterior estimates at the annual and/or inter-annual scale. Even if currently comparison between CH4 and N2O inversion estimates and NGHGIs is highly uncertain because of the large spread in the inversion results, TD inversions inferred from atmospheric observations represent the most independent data against which inventory totals can be compared. With anticipated improvements in atmospheric modeling and observations, as well as modeling of natural fluxes, TD inversions may arguably emerge as the most powerful tool for verifying emission inventories for CH4, N2O and other GHGs.
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