Global Carbon Budget 2021
Accurate assessment of anthropogenic carbon dioxide (CO2) emissions and their redistribution among the atmosphere, ocean, and terrestrial biosphere in a changing climate is critical to better understand the global carbon cycle, support the development of climate policies, and project future climate...
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Published in | Earth system science data Vol. 14; no. 4; pp. 1917 - 2005 |
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Main Authors | , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , |
Format | Journal Article |
Language | English |
Published |
Katlenburg-Lindau
Copernicus GmbH
26.04.2022
Copernicus Publications |
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Abstract | Accurate assessment of anthropogenic carbon dioxide (CO2) emissions and their redistribution among the atmosphere, ocean, and terrestrial biosphere in a changing climate is critical to better understand the global carbon cycle, support the development of climate policies, and project future climate change. Here we describe and synthesize datasets and methodology to quantify the five major components of the global carbon budget and their uncertainties. Fossil CO2 emissions (EFOS) are based on energy statistics and cement production data, while emissions from land-use change (ELUC), mainly deforestation, are based on land use and land-use change data and bookkeeping models. Atmospheric CO2 concentration is measured directly, and its growth rate (GATM) is computed from the annual changes in concentration. The ocean CO2 sink (SOCEAN) is estimated with global ocean biogeochemistry models and observation-based data products. The terrestrial CO2 sink (SLAND) is estimated with dynamic global vegetation models. The resulting carbon budget imbalance (BIM), the difference between the estimated total emissions and the estimated changes in the atmosphere, ocean, and terrestrial biosphere, is a measure of imperfect data and understanding of the contemporary carbon cycle. All uncertainties are reported as ±1σ. For the first time, an approach is shown to reconcile the difference in our ELUC estimate with the one from national greenhouse gas inventories, supporting the assessment of collective countries' climate progress. For the year 2020, EFOS declined by 5.4 % relative to 2019, with fossil emissions at 9.5 ± 0.5 GtC yr−1 (9.3 ± 0.5 GtC yr−1 when the cement carbonation sink is included), and ELUC was 0.9 ± 0.7 GtC yr−1, for a total anthropogenic CO2 emission of 10.2 ± 0.8 GtC yr−1 (37.4 ± 2.9 GtCO2). Also, for 2020, GATM was 5.0 ± 0.2 GtC yr−1 (2.4 ± 0.1 ppm yr−1), SOCEAN was 3.0 ± 0.4 GtC yr−1, and SLAND was 2.9 ± 1 GtC yr−1, with a BIM of −0.8 GtC yr−1. The global atmospheric CO2 concentration averaged over 2020 reached 412.45 ± 0.1 ppm. Preliminary data for 2021 suggest a rebound in EFOS relative to 2020 of +4.8 % (4.2 % to 5.4 %) globally. Overall, the mean and trend in the components of the global carbon budget are consistently estimated over the period 1959–2020, but discrepancies of up to 1 GtC yr−1 persist for the representation of annual to semi-decadal variability in CO2 fluxes. Comparison of estimates from multiple approaches and observations shows (1) a persistent large uncertainty in the estimate of land-use changes emissions, (2) a low agreement between the different methods on the magnitude of the land CO2 flux in the northern extra-tropics, and (3) a discrepancy between the different methods on the strength of the ocean sink over the last decade. This living data update documents changes in the methods and datasets used in this new global carbon budget and the progress in understanding of the global carbon cycle compared with previous publications of this dataset (Friedlingstein et al., 2020, 2019; Le Quéré et al., 2018b, a, 2016, 2015b, a, 2014, 2013). The data presented in this work are available at https://doi.org/10.18160/gcp-2021 (Friedlingstein et al., 2021). |
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AbstractList | Accurate assessment of anthropogenic carbon dioxide (CO2) emissions and their redistribution among the atmosphere, ocean, and terrestrial biosphere in a changing climate is critical to better understand the global carbon cycle, support the development of climate policies, and project future climate change. Here we describe and synthesize datasets and methodology to quantify the five major components of the global carbon budget and their uncertainties. Fossil CO2 emissions (EFOS) are based on energy statistics and cement production data, while emissions from land-use change (ELUC), mainly deforestation, are based on land use and land-use change data and bookkeeping models. Atmospheric CO2 concentration is measured directly, and its growth rate (GATM) is computed from the annual changes in concentration. The ocean CO2 sink (SOCEAN) is estimated with global ocean biogeochemistry models and observation-based data products. The terrestrial CO2 sink (SLAND) is estimated with dynamic global vegetation models. The resulting carbon budget imbalance (BIM), the difference between the estimated total emissions and the estimated changes in the atmosphere, ocean, and terrestrial biosphere, is a measure of imperfect data and understanding of the contemporary carbon cycle. All uncertainties are reported as ±1σ. For the first time, an approach is shown to reconcile the difference in our ELUC estimate with the one from national greenhouse gas inventories, supporting the assessment of collective countries' climate progress.For the year 2020, EFOS declined by 5.4 % relative to 2019, with fossil emissions at 9.5 ± 0.5 GtC yr-1 (9.3 ± 0.5 GtC yr-1 when the cement carbonation sink is included), and ELUC was 0.9 ± 0.7 GtC yr-1, for a total anthropogenic CO2 emission of 10.2 ± 0.8 GtC yr-1 (37.4 ± 2.9 GtCO2). Also, for 2020, GATM was 5.0 ± 0.2 GtC yr-1 (2.4 ± 0.1 ppm yr-1), SOCEAN was 3.0 ± 0.4 GtC yr-1, and SLAND was 2.9 ± 1 GtC yr-1, with a BIM of -0.8 GtC yr-1. The global atmospheric CO2 concentration averaged over 2020 reached 412.45 ± 0.1 ppm. Preliminary data for 2021 suggest a rebound in EFOS relative to 2020 of +4.8 % (4.2 % to 5.4 %) globally.Overall, the mean and trend in the components of the global carbon budget are consistently estimated over the period 1959–2020, but discrepancies of up to 1 GtC yr-1 persist for the representation of annual to semi-decadal variability in CO2 fluxes. Comparison of estimates from multiple approaches and observations shows (1) a persistent large uncertainty in the estimate of land-use changes emissions, (2) a low agreement between the different methods on the magnitude of the land CO2 flux in the northern extra-tropics, and (3) a discrepancy between the different methods on the strength of the ocean sink over the last decade. This living data update documents changes in the methods and datasets used in this new global carbon budget and the progress in understanding of the global carbon cycle compared with previous publications of this dataset (Friedlingstein et al., 2020, 2019; Le Quéré et al., 2018b, a, 2016, 2015b, a, 2014, 2013). The data presented in this work are available at 10.18160/gcp-2021 (Friedlingstein et al., 2021). Accurate assessment of anthropogenic carbon dioxide (CO.sub.2) emissions and their redistribution among the atmosphere, ocean, and terrestrial biosphere in a changing climate is critical to better understand the global carbon cycle, support the development of climate policies, and project future climate change. Here we describe and synthesize datasets and methodology to quantify the five major components of the global carbon budget and their uncertainties. Fossil CO.sub.2 emissions (E.sub.FOS) are based on energy statistics and cement production data, while emissions from land-use change (E.sub.LUC ), mainly deforestation, are based on land use and land-use change data and bookkeeping models. Atmospheric CO.sub.2 concentration is measured directly, and its growth rate (G.sub.ATM) is computed from the annual changes in concentration. The ocean CO.sub.2 sink (S.sub.OCEAN) is estimated with global ocean biogeochemistry models and observation-based data products. The terrestrial CO.sub.2 sink (S.sub.LAND) is estimated with dynamic global vegetation models. The resulting carbon budget imbalance (B.sub.IM ), the difference between the estimated total emissions and the estimated changes in the atmosphere, ocean, and terrestrial biosphere, is a measure of imperfect data and understanding of the contemporary carbon cycle. All uncertainties are reported as ±1Ï. For the first time, an approach is shown to reconcile the difference in our E.sub.LUC estimate with the one from national greenhouse gas inventories, supporting the assessment of collective countries' climate progress. Accurate assessment of anthropogenic carbon dioxide (CO2) emissions and their redistribution among the atmosphere, ocean, and terrestrial biosphere in a changing climate is critical to better understand the global carbon cycle, support the development of climate policies, and project future climate change. Here we describe and synthesize datasets and methodology to quantify the five major components of the global carbon budget and their uncertainties. Fossil CO2 emissions (EFOS) are based on energy statistics and cement production data, while emissions from land-use change (ELUC), mainly deforestation, are based on land use and land-use change data and bookkeeping models. Atmospheric CO2 concentration is measured directly, and its growth rate (GATM) is computed from the annual changes in concentration. The ocean CO2 sink (SOCEAN) is estimated with global ocean biogeochemistry models and observation-based data products. The terrestrial CO2 sink (SLAND) is estimated with dynamic global vegetation models. The resulting carbon budget imbalance (BIM), the difference between the estimated total emissions and the estimated changes in the atmosphere, ocean, and terrestrial biosphere, is a measure of imperfect data and understanding of the contemporary carbon cycle. All uncertainties are reported as ±1σ. For the first time, an approach is shown to reconcile the difference in our ELUC estimate with the one from national greenhouse gas inventories, supporting the assessment of collective countries' climate progress. For the year 2020, EFOS declined by 5.4 % relative to 2019, with fossil emissions at 9.5 ± 0.5 GtC yr-1 (9.3 ± 0.5 GtC yr-1 when the cement carbonation sink is included), and ELUC was 0.9 ± 0.7 GtC yr-1, for a total anthropogenic CO2 emission of 10.2 ± 0.8 GtC yr-1 (37.4 ± 2.9 GtCO2). Also, for 2020, GATM was 5.0 ± 0.2 GtC yr-1 (2.4 ± 0.1 ppm yr-1), SOCEAN was 3.0 ± 0.4 GtC yr-1, and SLAND was 2.9 ± 1 GtC yr-1, with a BIM of -0.8 GtC yr-1. The global atmospheric CO2 concentration averaged over 2020 reached 412.45 ± 0.1 ppm. Preliminary data for 2021 suggest a rebound in EFOS relative to 2020 of +4.8 % (4.2 % to 5.4 %) globally. Overall, the mean and trend in the components of the global carbon budget are consistently estimated over the period 1959-2020, but discrepancies of up to 1 GtC yr-1 persist for the representation of annual to semi-decadal variability in CO2 fluxes. Comparison of estimates from multiple approaches and observations shows (1) a persistent large uncertainty in the estimate of land-use changes emissions, (2) a low agreement between the different methods on the magnitude of the land CO2 flux in the northern extra-tropics, and (3) a discrepancy between the different methods on the strength of the ocean sink over the last decade. This living data update documents changes in the methods and datasets used in this new global carbon budget and the progress in understanding of the global carbon cycle compared with previous publications of this dataset (Friedlingstein et al., 2020, 2019; Le Quéré et al., 2018b, a, 2016, 2015b, a, 2014, 2013). The data presented in this work are available at https://doi.org/10.18160/gcp-2021 (Friedlingstein et al., 2021). Accurate assessment of anthropogenic carbon dioxide (CO 2 ) emissions and their redistribution among the atmosphere, ocean, and terrestrial biosphere in a changing climate is critical to better understand the global carbon cycle, support the development of climate policies, and project future climate change. Here we describe and synthesize datasets and methodology to quantify the five major components of the global carbon budget and their uncertainties. Fossil CO 2 emissions ( EFOS ) are based on energy statistics and cement production data, while emissions from land-use change ( ELUC ), mainly deforestation, are based on land use and land-use change data and bookkeeping models. Atmospheric CO 2 concentration is measured directly, and its growth rate ( GATM ) is computed from the annual changes in concentration. The ocean CO 2 sink ( SOCEAN ) is estimated with global ocean biogeochemistry models and observation-based data products. The terrestrial CO 2 sink ( SLAND ) is estimated with dynamic global vegetation models. The resulting carbon budget imbalance ( BIM ), the difference between the estimated total emissions and the estimated changes in the atmosphere, ocean, and terrestrial biosphere, is a measure of imperfect data and understanding of the contemporary carbon cycle. All uncertainties are reported as ± 1 σ . For the first time, an approach is shown to reconcile the difference in our ELUC estimate with the one from national greenhouse gas inventories, supporting the assessment of collective countries' climate progress. For the year 2020, EFOS declined by 5.4 % relative to 2019, with fossil emissions at 9.5 ± 0.5 GtC yr −1 (9.3 ± 0.5 GtC yr −1 when the cement carbonation sink is included), and ELUC was 0.9 ± 0.7 GtC yr −1 , for a total anthropogenic CO 2 emission of 10.2 ± 0.8 GtC yr −1 (37.4 ± 2.9 GtCO 2 ). Also, for 2020, GATM was 5.0 ± 0.2 GtC yr −1 (2.4 ± 0.1 ppm yr −1 ), SOCEAN was 3.0 ± 0.4 GtC yr −1 , and SLAND was 2.9 ± 1 GtC yr −1 , with a BIM of − 0.8 GtC yr −1 . The global atmospheric CO 2 concentration averaged over 2020 reached 412.45 ± 0.1 ppm. Preliminary data for 2021 suggest a rebound in EFOS relative to 2020 of + 4.8 % (4.2 % to 5.4 %) globally. Overall, the mean and trend in the components of the global carbon budget are consistently estimated over the period 1959–2020, but discrepancies of up to 1 GtC yr −1 persist for the representation of annual to semi-decadal variability in CO 2 fluxes. Comparison of estimates from multiple approaches and observations shows (1) a persistent large uncertainty in the estimate of land-use changes emissions, (2) a low agreement between the different methods on the magnitude of the land CO 2 flux in the northern extra-tropics, and (3) a discrepancy between the different methods on the strength of the ocean sink over the last decade. This living data update documents changes in the methods and datasets used in this new global carbon budget and the progress in understanding of the global carbon cycle compared with previous publications of this dataset (Friedlingstein et al., 2020, 2019; Le Quéré et al., 2018b, a, 2016, 2015b, a, 2014, 2013). The data presented in this work are available at https://doi.org/10.18160/gcp-2021 (Friedlingstein et al., 2021). Accurate assessment of anthropogenic carbon dioxide (CO2) emissions and their redistribution among the atmosphere, ocean, and terrestrial biosphere in a changing climate is critical to better understand the global carbon cycle, support the development of climate policies, and project future climate change. Here we describe and synthesize datasets and methodology to quantify the five major components of the global carbon budget and their uncertainties. Fossil CO2 emissions (EFOS) are based on energy statistics and cement production data, while emissions from land-use change (ELUC), mainly deforestation, are based on land use and land-use change data and bookkeeping models. Atmospheric CO2 concentration is measured directly, and its growth rate (GATM) is computed from the annual changes in concentration. The ocean CO2 sink (SOCEAN) is estimated with global ocean biogeochemistry models and observation-based data products. The terrestrial CO2 sink (SLAND) is estimated with dynamic global vegetation models. The resulting carbon budget imbalance (BIM), the difference between the estimated total emissions and the estimated changes in the atmosphere, ocean, and terrestrial biosphere, is a measure of imperfect data and understanding of the contemporary carbon cycle. All uncertainties are reported as ±1σ. For the first time, an approach is shown to reconcile the difference in our ELUC estimate with the one from national greenhouse gas inventories, supporting the assessment of collective countries' climate progress. For the year 2020, EFOS declined by 5.4 % relative to 2019, with fossil emissions at 9.5 ± 0.5 GtC yr−1 (9.3 ± 0.5 GtC yr−1 when the cement carbonation sink is included), and ELUC was 0.9 ± 0.7 GtC yr−1, for a total anthropogenic CO2 emission of 10.2 ± 0.8 GtC yr−1 (37.4 ± 2.9 GtCO2). Also, for 2020, GATM was 5.0 ± 0.2 GtC yr−1 (2.4 ± 0.1 ppm yr−1), SOCEAN was 3.0 ± 0.4 GtC yr−1, and SLAND was 2.9 ± 1 GtC yr−1, with a BIM of −0.8 GtC yr−1. The global atmospheric CO2 concentration averaged over 2020 reached 412.45 ± 0.1 ppm. Preliminary data for 2021 suggest a rebound in EFOS relative to 2020 of +4.8 % (4.2 % to 5.4 %) globally. Overall, the mean and trend in the components of the global carbon budget are consistently estimated over the period 1959–2020, but discrepancies of up to 1 GtC yr−1 persist for the representation of annual to semi-decadal variability in CO2 fluxes. Comparison of estimates from multiple approaches and observations shows (1) a persistent large uncertainty in the estimate of land-use changes emissions, (2) a low agreement between the different methods on the magnitude of the land CO2 flux in the northern extra-tropics, and (3) a discrepancy between the different methods on the strength of the ocean sink over the last decade. This living data update documents changes in the methods and datasets used in this new global carbon budget and the progress in understanding of the global carbon cycle compared with previous publications of this dataset (Friedlingstein et al., 2020, 2019; Le Quéré et al., 2018b, a, 2016, 2015b, a, 2014, 2013). The data presented in this work are available at https://doi.org/10.18160/gcp-2021 (Friedlingstein et al., 2021). Accurate assessment of anthropogenic carbon dioxide (CO2) emissions and their redistribution among the atmosphere, ocean, and terrestrial biosphere in a changing climate is critical to better understand the global carbon cycle, support the development of climate policies, and project future climate change. Here we describe and synthesize datasets and methodology to quantify the five major components of the global carbon budget and their uncertainties. Fossil CO2 emissions (EFOS) are based on energy statistics and cement production data, while emissions from land-use change (ELUC), mainly deforestation, are based on land use and land-use change data and bookkeeping models. Atmospheric CO2 concentration is measured directly, and its growth rate (GATM) is computed from the annual changes in concentration. The ocean CO2 sink (SOCEAN) is estimated with global ocean biogeochemistry models and observation-based data products. The terrestrial CO2 sink (SLAND) is estimated with dynamic global vegetation models. The resulting carbon budget imbalance (BIM), the difference between the estimated total emissions and the estimated changes in the atmosphere, ocean, and terrestrial biosphere, is a measure of imperfect data and understanding of the contemporary carbon cycle. All uncertainties are reported as ±1σ. For the first time, an approach is shown to reconcile the difference in our ELUC estimate with the one from national greenhouse gas inventories, supporting the assessment of collective countries' climate progress. For the year 2020, EFOS declined by 5.4 % relative to 2019, with fossil emissions at 9.5 ± 0.5 GtC yr−1 (9.3 ± 0.5 GtC yr−1 when the cement carbonation sink is included), and ELUC was 0.9 ± 0.7 GtC yr−1, for a total anthropogenic CO2 emission of 10.2 ± 0.8 GtC yr−1 (37.4 ± 2.9 GtCO2). Also, for 2020, GATM was 5.0 ± 0.2 GtC yr−1 (2.4 ± 0.1 ppm yr−1), SOCEAN was 3.0 ± 0.4 GtC yr−1, and SLAND was 2.9 ± 1 GtC yr−1, with a BIM of −0.8 GtC yr−1. The global atmospheric CO2 concentration averaged over 2020 reached 412.45 ± 0.1 ppm. Preliminary data for 2021 suggest a rebound in EFOS relative to 2020 of +4.8 % (4.2 % to 5.4 %) globally. Overall, the mean and trend in the components of the global carbon budget are consistently estimated over the period 1959–2020, but discrepancies of up to 1 GtC yr−1 persist for the representation of annual to semi-decadal variability in CO2 fluxes. Comparison of estimates from multiple approaches and observations shows (1) a persistent large uncertainty in the estimate of land-use changes emissions, (2) a low agreement between the different methods on the magnitude of the land CO2 flux in the northern extra-tropics, and (3) a discrepancy between the different methods on the strength of the ocean sink over the last decade. This living data update documents changes in the methods and datasets used in this new global carbon budget and the progress in understanding of the global carbon cycle compared with previous publications of this dataset (Friedlingstein et al., 2020, 2019; Le Quéré et al., 2018b, a, 2016, 2015b, a, 2014, 2013). The data presented in this work are available at https://doi.org/10.18160/gcp-2021 (Friedlingstein et al., 2021). Accurate assessment of anthropogenic carbon dioxide (CO.sub.2) emissions and their redistribution among the atmosphere, ocean, and terrestrial biosphere in a changing climate is critical to better understand the global carbon cycle, support the development of climate policies, and project future climate change. Here we describe and synthesize datasets and methodology to quantify the five major components of the global carbon budget and their uncertainties. Fossil CO.sub.2 emissions (E.sub.FOS) are based on energy statistics and cement production data, while emissions from land-use change (E.sub.LUC ), mainly deforestation, are based on land use and land-use change data and bookkeeping models. Atmospheric CO.sub.2 concentration is measured directly, and its growth rate (G.sub.ATM) is computed from the annual changes in concentration. The ocean CO.sub.2 sink (S.sub.OCEAN) is estimated with global ocean biogeochemistry models and observation-based data products. The terrestrial CO.sub.2 sink (S.sub.LAND) is estimated with dynamic global vegetation models. The resulting carbon budget imbalance (B.sub.IM ), the difference between the estimated total emissions and the estimated changes in the atmosphere, ocean, and terrestrial biosphere, is a measure of imperfect data and understanding of the contemporary carbon cycle. All uncertainties are reported as ±1Ï. For the first time, an approach is shown to reconcile the difference in our E.sub.LUC estimate with the one from national greenhouse gas inventories, supporting the assessment of collective countries' climate progress. For the year 2020, E.sub.FOS declined by 5.4 % relative to 2019, with fossil emissions at 9.5 ± 0.5 GtC yr.sup.-1 (9.3 ± 0.5 GtC yr.sup.-1 when the cement carbonation sink is included), and E.sub.LUC was 0.9 ± 0.7 GtC yr.sup.-1, for a total anthropogenic CO.sub.2 emission of 10.2 ± 0.8 GtC yr.sup.-1 (37.4 ± 2.9 GtCO.sub.2). Also, for 2020, G.sub.ATM was 5.0 ± 0.2 GtC yr.sup.-1 (2.4 ± 0.1 ppm yr.sup.-1 ), S.sub.OCEAN was 3.0 ± 0.4 GtC yr.sup.-1, and S.sub.LAND was 2.9 ± 1 GtC yr.sup.-1, with a B.sub.IM of -0.8 GtC yr.sup.-1 . The global atmospheric CO.sub.2 concentration averaged over 2020 reached 412.45 ± 0.1 ppm. Preliminary data for 2021 suggest a rebound in E.sub.FOS relative to 2020 of +4.8 % (4.2 % to 5.4 %) globally. Overall, the mean and trend in the components of the global carbon budget are consistently estimated over the period 1959-2020, but discrepancies of up to 1 GtC yr.sup.-1 persist for the representation of annual to semi-decadal variability in CO.sub.2 fluxes. Comparison of estimates from multiple approaches and observations shows (1) a persistent large uncertainty in the estimate of land-use changes emissions, (2) a low agreement between the different methods on the magnitude of the land CO.sub.2 flux in the northern extra-tropics, and (3) a discrepancy between the different methods on the strength of the ocean sink over the last decade. This living data update documents changes in the methods and datasets used in this new global carbon budget and the progress in understanding of the global carbon cycle compared with previous publications of this dataset (Friedlingstein et al., 2020, 2019; Le Quéré et al., 2018b, a, 2016, 2015b, a, 2014, 2013). The data presented in this work are available at |
Audience | Academic |
Author | Tanhua, Toste Feely, Richard A. Chevallier, Frédéric Tian, Hanqin Gregor, Luke Wiltshire, Andrew J. Jones, Matthew W. Munro, David R. Lauvset, Siv K. Chini, Louise P. Currie, Kim I. Ilyina, Tatiana Tans, Pieter P. Gruber, Nicolas Knauer, Jürgen Poulter, Benjamin Peters, Wouter McGuire, Patrick C. Houghton, Richard A. Harris, Ian Luijkx, Ingrid T. Gilfillan, Dennis Rödenbeck, Christian Watson, Andrew J. Wanninkhof, Rik Peters, Glen P. Djeutchouang, Laique M. Resplandy, Laure Liu, Junjie Jackson, Rob B. Chau, Thi Tuyet Trang Hurtt, George C. Robertson, Eddy Evans, Wiley Jain, Atul Marland, Gregg Sweeney, Colm Dou, Xinyu Le Quéré, Corinne Zaehle, Sönke Friedlingstein, Pierre Becker, Meike Korsbakken, Jan Ivar Sitch, Stephen Feng, Liang Kato, Etsushi Yuan, Wenping O'Sullivan, Michael Körtzinger, Arne Rehder, Gregor Andrew, Robbie M. Decharme, Bertrand Pierrot, Denis Ono, Tsuneo Nabel, Julia E. M. S. Kennedy, Daniel Lefèvre, Nathalie Lienert, Sebastian Yue, Chao Tubiello, Francesco Zeng, Jiye Bopp, Laurent Gkritzalis, Thanos Ciais, Philippe Rosan, Thais |
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Currie, Kim I. – sequence: 26 givenname: Bertrand orcidid: 0000-0002-8661-1464 surname: Decharme fullname: Decharme, Bertrand – sequence: 27 givenname: Laique M. surname: Djeutchouang fullname: Djeutchouang, Laique M. – sequence: 28 givenname: Xinyu orcidid: 0000-0001-7783-6971 surname: Dou fullname: Dou, Xinyu – sequence: 29 givenname: Wiley orcidid: 0000-0002-5450-0903 surname: Evans fullname: Evans, Wiley – sequence: 30 givenname: Richard A. surname: Feely fullname: Feely, Richard A. – sequence: 31 givenname: Liang surname: Feng fullname: Feng, Liang – sequence: 32 givenname: Thomas orcidid: 0000-0003-4882-2647 surname: Gasser fullname: Gasser, Thomas – sequence: 33 givenname: Dennis surname: Gilfillan fullname: Gilfillan, Dennis – sequence: 34 givenname: Thanos surname: Gkritzalis fullname: Gkritzalis, Thanos – sequence: 35 givenname: Giacomo surname: Grassi fullname: Grassi, Giacomo – sequence: 36 givenname: Luke orcidid: 0000-0001-6071-1857 surname: Gregor fullname: Gregor, Luke – sequence: 37 givenname: Nicolas orcidid: 0000-0002-2085-2310 surname: Gruber fullname: Gruber, Nicolas – sequence: 38 givenname: Özgür orcidid: 0000-0002-0646-5760 surname: Gürses fullname: Gürses, Özgür – sequence: 39 givenname: Ian surname: Harris fullname: Harris, Ian – sequence: 40 givenname: Richard A. orcidid: 0000-0002-3298-7028 surname: Houghton fullname: Houghton, Richard A. – sequence: 41 givenname: George C. orcidid: 0000-0001-7278-202X surname: Hurtt fullname: Hurtt, George C. – sequence: 42 givenname: Yosuke orcidid: 0000-0001-5711-1375 surname: Iida fullname: Iida, Yosuke – sequence: 43 givenname: Tatiana orcidid: 0000-0002-3475-4842 surname: Ilyina fullname: Ilyina, Tatiana – sequence: 44 givenname: Ingrid T. orcidid: 0000-0002-3990-6737 surname: Luijkx fullname: Luijkx, Ingrid T. – sequence: 45 givenname: Atul orcidid: 0000-0002-4051-3228 surname: Jain fullname: Jain, Atul – sequence: 46 givenname: Steve D. orcidid: 0000-0003-0522-9851 surname: Jones fullname: Jones, Steve D. – sequence: 47 givenname: Etsushi orcidid: 0000-0001-8814-804X surname: Kato fullname: Kato, Etsushi – sequence: 48 givenname: Daniel surname: Kennedy fullname: Kennedy, Daniel – sequence: 49 givenname: Kees orcidid: 0000-0003-2714-7507 surname: Klein Goldewijk fullname: Klein Goldewijk, Kees – sequence: 50 givenname: Jürgen orcidid: 0000-0002-4947-7067 surname: Knauer fullname: Knauer, Jürgen – sequence: 51 givenname: Jan Ivar orcidid: 0000-0002-2939-9778 surname: Korsbakken fullname: Korsbakken, Jan Ivar – sequence: 52 givenname: Arne orcidid: 0000-0002-8181-3593 surname: Körtzinger fullname: Körtzinger, Arne – sequence: 53 givenname: Peter orcidid: 0000-0002-7398-3293 surname: Landschützer fullname: Landschützer, Peter – sequence: 54 givenname: Siv K. orcidid: 0000-0001-8498-4067 surname: Lauvset fullname: Lauvset, Siv K. – sequence: 55 givenname: Nathalie surname: Lefèvre fullname: Lefèvre, Nathalie – sequence: 56 givenname: Sebastian surname: Lienert fullname: Lienert, Sebastian – sequence: 57 givenname: Junjie orcidid: 0000-0002-7184-6594 surname: Liu fullname: Liu, Junjie – sequence: 58 givenname: Gregg surname: Marland fullname: Marland, Gregg – sequence: 59 givenname: Patrick C. orcidid: 0000-0001-6592-4966 surname: McGuire fullname: McGuire, Patrick C. – sequence: 60 givenname: Joe R. orcidid: 0000-0002-9414-064X surname: Melton fullname: Melton, Joe R. – sequence: 61 givenname: David R. orcidid: 0000-0002-1373-7402 surname: Munro fullname: Munro, David R. – sequence: 62 givenname: Julia E. M. S. orcidid: 0000-0002-8122-5206 surname: Nabel fullname: Nabel, Julia E. M. S. – sequence: 63 givenname: Shin-Ichiro orcidid: 0000-0002-3870-1721 surname: Nakaoka fullname: Nakaoka, Shin-Ichiro – sequence: 64 givenname: Yosuke orcidid: 0000-0002-7600-9816 surname: Niwa fullname: Niwa, Yosuke – sequence: 65 givenname: Tsuneo orcidid: 0000-0003-3472-5731 surname: Ono fullname: Ono, Tsuneo – sequence: 66 givenname: Denis orcidid: 0000-0002-0374-3825 surname: Pierrot fullname: Pierrot, Denis – sequence: 67 givenname: Benjamin orcidid: 0000-0002-9493-8600 surname: Poulter fullname: Poulter, Benjamin – sequence: 68 givenname: Gregor orcidid: 0000-0002-0597-9989 surname: Rehder fullname: Rehder, Gregor – sequence: 69 givenname: Laure orcidid: 0000-0002-1212-3943 surname: Resplandy fullname: Resplandy, Laure – sequence: 70 givenname: Eddy surname: Robertson fullname: Robertson, Eddy – sequence: 71 givenname: Christian orcidid: 0000-0001-6011-6249 surname: Rödenbeck fullname: Rödenbeck, Christian – sequence: 72 givenname: Thais M. orcidid: 0000-0003-0155-1739 surname: Rosan fullname: Rosan, Thais M. – sequence: 73 givenname: Jörg orcidid: 0000-0002-7525-6882 surname: Schwinger fullname: Schwinger, Jörg – sequence: 74 givenname: Clemens orcidid: 0000-0003-4048-3011 surname: Schwingshackl fullname: Schwingshackl, Clemens – sequence: 75 givenname: Roland orcidid: 0000-0002-2571-2114 surname: Séférian fullname: Séférian, Roland – sequence: 76 givenname: Adrienne J. orcidid: 0000-0002-7414-7035 surname: Sutton fullname: Sutton, Adrienne J. – sequence: 77 givenname: Colm orcidid: 0000-0002-4517-0797 surname: Sweeney fullname: Sweeney, Colm – sequence: 78 givenname: Toste orcidid: 0000-0002-0313-2557 surname: Tanhua fullname: Tanhua, Toste – sequence: 79 givenname: Pieter P. surname: Tans fullname: Tans, Pieter P. – sequence: 80 givenname: Hanqin orcidid: 0000-0002-1806-4091 surname: Tian fullname: Tian, Hanqin – sequence: 81 givenname: Bronte orcidid: 0000-0001-9385-3827 surname: Tilbrook fullname: Tilbrook, Bronte – sequence: 82 givenname: Francesco orcidid: 0000-0003-4617-4690 surname: Tubiello fullname: Tubiello, Francesco – sequence: 83 givenname: Guido R. orcidid: 0000-0001-9042-8630 surname: van der Werf fullname: van der Werf, Guido R. – sequence: 84 givenname: Nicolas orcidid: 0000-0002-3397-7948 surname: Vuichard fullname: Vuichard, Nicolas – sequence: 85 givenname: Chisato surname: Wada fullname: Wada, Chisato – sequence: 86 givenname: Rik surname: Wanninkhof fullname: Wanninkhof, Rik – sequence: 87 givenname: Andrew J. orcidid: 0000-0002-9654-8147 surname: Watson fullname: Watson, Andrew J. – sequence: 88 givenname: David surname: Willis fullname: Willis, David – sequence: 89 givenname: Andrew J. surname: Wiltshire fullname: Wiltshire, Andrew J. – sequence: 90 givenname: Wenping surname: Yuan fullname: Yuan, Wenping – sequence: 91 givenname: Chao orcidid: 0000-0003-0026-237X surname: Yue fullname: Yue, Chao – sequence: 92 givenname: Xu orcidid: 0000-0002-8861-8192 surname: Yue fullname: Yue, Xu – sequence: 93 givenname: Sönke orcidid: 0000-0001-5602-7956 surname: Zaehle fullname: Zaehle, Sönke – sequence: 94 givenname: Jiye surname: Zeng fullname: Zeng, Jiye |
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