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

被引:10
|
作者
Petrescu, Ana Maria Roxana [1 ,28 ]
Qiu, Chunjing [2 ,28 ]
McGrath, Matthew J. [2 ,28 ]
Peylin, Philippe [2 ,28 ]
Peters, Glen P. [3 ,28 ]
Ciais, Philippe [2 ,28 ]
Thompson, Rona L. [4 ,28 ]
Tsuruta, Aki [5 ,28 ]
Brunner, Dominik [6 ,28 ]
Kuhnert, Matthias [7 ,28 ]
Matthews, Bradley [8 ,28 ]
Palmer, Paul I. [9 ,28 ]
Tarasova, Oksana [10 ,28 ]
Regnier, Pierre [11 ,28 ]
Lauerwald, Ronny [12 ,28 ]
Bastviken, David [13 ,28 ]
Hoeglund-Isaksson, Lena [14 ,28 ]
Winiwarter, Wilfried [14 ,15 ,28 ]
Etiope, Giuseppe [16 ,28 ]
Aalto, Tuula [5 ,28 ]
Balsamo, Gianpaolo [17 ,28 ]
Bastrikov, Vladislav [18 ,28 ]
Berchet, Antoine [2 ,28 ]
Brockmann, Patrick [2 ,28 ]
Ciotoli, Giancarlo [19 ,28 ]
Conchedda, Giulia [20 ,28 ]
Crippa, Monica [21 ,28 ]
Dentener, Frank [21 ,28 ]
Zwaaftink, Christine D. Groot [28 ]
Guizzardi, Diego [21 ,28 ]
Guenther, Dirk [22 ,28 ]
Haussaire, Jean-Matthieu [6 ,28 ]
Houweling, Sander [1 ,28 ]
Janssens-Maenhout, Greet [21 ,28 ]
Kouyate, Massaer [28 ]
Leip, Adrian [21 ,28 ,35 ]
Leppanen, Antti [23 ]
Lugato, Emanuele [21 ]
Maisonnier, Manon [11 ]
Manning, Alistair J. [24 ]
Markkanen, Tiina [5 ]
McNorton, Joe [17 ]
Muntean, Marilena [21 ]
Oreggioni, Gabriel D. [21 ,34 ]
Patra, Prabir K. [25 ]
Perugini, Lucia [26 ]
Pison, Isabelle [2 ]
Raivonen, Maarit T. [23 ]
Saunois, Marielle [2 ]
Segers, Arjo J. [27 ]
机构
[1] Vrije Univ Amsterdam, Dept Earth Sci, NL-1081 HV Amsterdam, Netherlands
[2] Lab Sci Climat & Environm, F-91190 Gif Sur Yvette, France
[3] Ctr Int Climate Res CICERO, Oslo, Norway
[4] Norwegian Inst Air Res NILU, Kjeller, Norway
[5] Finnish Meteorol Inst, POB 503, Helsinki 00101, Finland
[6] Swiss Fed Labs Mat Sci & Technol EMPA, CH-8600 Dubendorf, Switzerland
[7] Univ Aberdeen, Inst Biol & Environm Sci, 23 St Machar Dr, Aberdeen AB24 3UU, Scotland
[8] Umweltbundesamt GmbH, Climate Change Mitigat & Emiss Inventories, A-1090 Vienna, Austria
[9] Univ Edinburgh, Sch Geosci, Edinburgh, Midlothian, Scotland
[10] World Meteorol Org WMO, Sci & Innovat Dept, Geneva, Switzerland
[11] Univ Libre Bruxelles, Dept Geosci, Biogeochem & Modeling Earth Syst, Environm & Soc, CP160-02, B-1050 Brussels, Belgium
[12] Univ Paris Saclay, INRAE, AgroParisTech, UMR ECOSYS, F-9120 Palaiseau, France
[13] Linkoping Univ, Dept Themat Studies, Environm Change, Linkoping, Sweden
[14] Int Inst Appl Syst Anal IIASA, A-2361 Laxenburg, Austria
[15] Univ Zielona, Inst Environm Engn, PL-65417 Zielona Gora, Poland
[16] Ist Nazl Geofis & Vulcanol, Sez Roma 2, Via V Murata 605, Rome, Italy
[17] European Ctr Medium Range Weather Forecasts ECMWF, Reading RG2 9AX, Berks, England
[18] Sci Partners, F-75010 Paris, France
[19] CNR, Ist Geol Ambientale & Geoingn, Via Salaria km 29300, I-00015 Monterotondo, Rome, Italy
[20] Food & Agr Org United Nations FAO, Stat Div, I-00153 Rome, Italy
[21] European Commiss, Joint Res Ctr, I-21027 Ispra, VA, Italy
[22] Umweltbundesamt UBA, D-14193 Berlin, Germany
[23] Univ Helsinki, Inst Atmospher & Earth Syst Res Phys, Fac Sci, Helsinki 00560, Finland
[24] Hadley Ctr, Met Off, Exeter EX1 3PB, England
[25] JAMSTEC, Res Inst Global Change, Yokohama 2360001, Japan
[26] Ctr Euro Mediterraneo Cambiamenti Climat CMCC, Viterbo, Italy
[27] TNO, Dept Climate Air & Sustainabil, Princetonlaan 6, NL-3584 CB Utrecht, Netherlands
[28] Uni Syst, Milan, Italy
[29] Auburn Univ, Int Ctr Climate & Global Change, Sch Forestry & Wildlife Sci, Auburn, AL 36849 USA
[30] Univ Helsinki, Inst Atmospher & Earth Syst Res Forest Sci, Fac Agr & Forestry, Helsinki, Finland
[31] Univ Leeds, Inst Climate & Atmospher Sci, Leeds, W Yorkshire, England
[32] Univ Leeds, Natl Ctr Earth Observat, Leeds, W Yorkshire, England
[33] Max Planck Inst Biogeochem MPI BGC, Jena, Germany
[34] Imperial Coll, Ctr Environm Policy, London SW7 1NE, England
[35] European Commiss, DG Res & Innovat, B-1050 Brussels, Belgium
基金
欧洲研究理事会; 欧盟地平线“2020”;
关键词
GREENHOUSE-GAS EMISSIONS; PARTICLE DISPERSION MODEL; LAST GLACIAL MAXIMUM; METHANE EMISSIONS; ATMOSPHERIC METHANE; TERRESTRIAL ECOSYSTEMS; TECHNICAL NOTE; SPATIOTEMPORAL DYNAMICS; INVERSION FRAMEWORK; NATURAL WETLANDS;
D O I
10.5194/essd-15-1197-2023
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
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 TgCH(4) yr(-1) (EDGARv6.0, last year 2018) and 18.4 TgCH(4) yr(-1) (GAINS, last year 2015), close to the NGHGI estimates of 17 :5 +/- 2 :1 TgCH(4) 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 TgCH(4) yr(-1). Coarser-resolution global-scale TD inversions result in emission estimates of 23 and 24 TgCH(4) 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 TgCH(4) 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 TgN(2)Oyr(-1), close to the NGHGI data (0 :8 +/- 55% TgN(2)Oyr(-1)). Over the same period, the mean of TD global and regional inversions was 1.4 TgN(2)Oyr(-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 C 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. The referenced dataset srelated to figures are visualized at https://doi.org/10.5281/zenodo.7553800 (Petrescu et al., 2023).
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收藏
页码:1197 / 1268
页数:72
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