Global Carbon Budget 2022
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. 11; pp. 4811 - 4900 |
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| Main Authors | , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , |
| Format | Journal Article |
| Language | English |
| Published |
Goddard Space Flight Center
Copernicus.org (Germany)
11.11.2022
Copernicus GmbH Copernicus Publications |
| Subjects | |
| Online Access | Get full text |
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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 data sets and methodologies 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 year 2021, EFOS increased by 5.1 % relative to 2020, with fossil emissions at 10.1 ± 0.5 GtC yr−1 (9.9 ± 0.5 GtC yr−1 when the cement carbonation sink is included), and ELUC was 1.1 ± 0.7 GtC yr−1, for a total anthropogenic CO2 emission (including the cement carbonation sink) of 10.9 ± 0.8 GtC yr−1 (40.0 ± 2.9 GtCO2). Also, for 2021, GATM was 5.2 ± 0.2 GtC yr−1 (2.5 ± 0.1 ppm yr−1), SOCEAN was 2.9 ± 0.4 GtC yr−1, and SLAND was 3.5 ± 0.9 GtC yr−1, with a BIM of −0.6 GtC yr−1 (i.e. the total estimated sources were too low or sinks were too high). The global atmospheric CO2 concentration averaged over 2021 reached 414.71 ± 0.1 ppm. Preliminary data for 2022 suggest an increase in EFOS relative to 2021 of +1.0 % (0.1 % to 1.9 %) globally and atmospheric CO2 concentration reaching 417.2 ppm, more than 50 % above pre-industrial levels (around 278 ppm). Overall, the mean and trend in the components of the global carbon budget are consistently estimated over the period 1959–2021, 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 change emissions, (2) a low agreement between the different methods on the magnitude of the land CO2 flux in the northern extratropics, 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 data sets used in this new global carbon budget and the progress in understanding of the global carbon cycle compared with previous publications of this data set. The data presented in this work are available at https://doi.org/10.18160/GCP-2022 (Friedlingstein et al., 2022b). |
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| AbstractList | 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 data sets and methodologies 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. 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 data sets and methodologies 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 year 2021, E.sub.FOS increased by 5.1 % relative to 2020, with fossil emissions at 10.1 ± 0.5 GtC yr.sup.-1 (9.9 ± 0.5 GtC yr.sup.-1 when the cement carbonation sink is included), and E.sub.LUC was 1.1 ± 0.7 GtC yr.sup.-1, for a total anthropogenic CO.sub.2 emission (including the cement carbonation sink) of 10.9 ± 0.8 GtC yr.sup.-1 (40.0 ± 2.9 GtCO.sub.2). Also, for 2021, G.sub.ATM was 5.2 ± 0.2 GtC yr.sup.-1 (2.5 ± 0.1 ppm yr.sup.-1 ), S.sub.OCEAN was 2.9 ± 0.4 GtC yr.sup.-1, and S.sub.LAND was 3.5 ± 0.9 GtC yr.sup.-1, with a B.sub.IM of -0.6 GtC yr.sup.-1 (i.e. the total estimated sources were too low or sinks were too high). The global atmospheric CO.sub.2 concentration averaged over 2021 reached 414.71 ± 0.1 ppm. Preliminary data for 2022 suggest an increase in E.sub.FOS relative to 2021 of +1.0 % (0.1 % to 1.9 %) globally and atmospheric CO.sub.2 concentration reaching 417.2 ppm, more than 50 % above pre-industrial levels (around 278 ppm). Overall, the mean and trend in the components of the global carbon budget are consistently estimated over the period 1959-2021, 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 change emissions, (2) a low agreement between the different methods on the magnitude of the land CO.sub.2 flux in the northern extratropics, 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 data sets used in this new global carbon budget and the progress in understanding of the global carbon cycle compared with previous publications of this data set. The data presented in this work are available at 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 data sets and methodologies 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 year 2021, EFOS increased by 5.1 % relative to 2020, with fossil emissions at 10.1 ± 0.5 GtC yr—1 (9.9 ± 0.5 GtC yr—1 when the cement carbonation sink is included), and ELUC was 1.1 ± 0.7 GtC yr—1, for a total anthropogenic CO2 emission (including the cement carbonation sink) of 10.9 ± 0.8 GtC yr—1 (40.0 ± 2.9 GtCO2). Also, for 2021, GATM was 5.2 ± 0.2 GtC yr—1 (2.5 ± 0.1 ppm yr—1), SOCEAN was 2.9 ± 0.4 GtC yr—1, and SLAND was 3.5 ± 0.9 GtC yr—1, with a BIM of —0.6 GtC yr—1 (i.e. the total estimated sources were too low or sinks were too high). The global atmospheric CO2 concentration averaged over 2021 reached 414.71 ± 0.1 ppm. Preliminary data for 2022 suggest an increase in EFOS relative to 2021 of +1.0 % (0.1 % to 1.9 %) globally and atmospheric CO2 concentration reaching 417.2 ppm, more than 50 % above pre-industrial levels (around 278 ppm). Overall, the mean and trend in the components of the global carbon budget are consistently estimated over the period 1959–2021, 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 change emissions, (2) a low agreement between the different methods on the magnitude of the land CO2 flux in the northern extratropics, 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 data sets used in this new global carbon budget and the progress in understanding of the global carbon cycle compared with previous publications of this data set. The data presented in this work are available at https://doi.org/10.18160/GCP-2022 (Friedlingstein et al., 2022b). 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 data sets and methodologies 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 year 2021, EFOS increased by 5.1 % relative to 2020, with fossil emissions at 10.1 ± 0.5 GtC yr−1 (9.9 ± 0.5 GtC yr−1 when the cement carbonation sink is included), and ELUC was 1.1 ± 0.7 GtC yr−1, for a total anthropogenic CO2 emission (including the cement carbonation sink) of 10.9 ± 0.8 GtC yr−1 (40.0 ± 2.9 GtCO2). Also, for 2021, GATM was 5.2 ± 0.2 GtC yr−1 (2.5 ± 0.1 ppm yr−1), SOCEAN was 2.9 ± 0.4 GtC yr−1, and SLAND was 3.5 ± 0.9 GtC yr−1, with a BIM of −0.6 GtC yr−1 (i.e. the total estimated sources were too low or sinks were too high). The global atmospheric CO2 concentration averaged over 2021 reached 414.71 ± 0.1 ppm. Preliminary data for 2022 suggest an increase in EFOS relative to 2021 of +1.0 % (0.1 % to 1.9 %) globally and atmospheric CO2 concentration reaching 417.2 ppm, more than 50 % above pre-industrial levels (around 278 ppm). Overall, the mean and trend in the components of the global carbon budget are consistently estimated over the period 1959–2021, 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 change emissions, (2) a low agreement between the different methods on the magnitude of the land CO2 flux in the northern extratropics, 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 data sets used in this new global carbon budget and the progress in understanding of the global carbon cycle compared with previous publications of this data set. The data presented in this work are available at https://doi.org/10.18160/GCP-2022 (Friedlingstein et al., 2022b). 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 data sets and methodologies 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 year 2021, EFOS increased by 5.1 % relative to 2020, with fossil emissions at 10.1 ± 0.5 GtC yr-1 (9.9 ± 0.5 GtC yr-1 when the cement carbonation sink is included), and ELUC was 1.1 ± 0.7 GtC yr-1, for a total anthropogenic CO2 emission (including the cement carbonation sink) of 10.9 ± 0.8 GtC yr-1 (40.0 ± 2.9 GtCO2). Also, for 2021, GATM was 5.2 ± 0.2 GtC yr-1 (2.5 ± 0.1 ppm yr-1), SOCEAN was 2.9 ± 0.4 GtC yr-1, and SLAND was 3.5 ± 0.9 GtC yr-1, with aBIM of -0.6 GtC yr-1 (i.e. the total estimated sources were too low or sinks were too high). The global atmospheric CO2 concentration averaged over 2021 reached 414.71 ± 0.1 ppm. Preliminary data for 2022 suggest an increase in EFOS relative to 2021 of +1.0 % (0.1 % to 1.9 %) globally and atmospheric CO2 concentration reaching 417.2 ppm, more than 50 % above pre-industrial levels (around 278 ppm). Overall, the mean and trend in the components of the global carbon budget are consistently estimated over the period 1959–2021, 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 change emissions, (2) a low agreement between the different methods on the magnitude of the land CO2 flux in the northern extratropics, 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 data sets used in this new global carbon budget and the progress in understanding of the global carbon cycle compared with previous publications of this data set. The data presented in this work are available at 10.18160/GCP-2022 (Friedlingstein et al., 2022b). 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 data sets and methodologies 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 year 2021, EFOS increased by 5.1 % relative to 2020, with fossil emissions at 10.1 ± 0.5 GtC yr−1 (9.9 ± 0.5 GtC yr−1 when the cement carbonation sink is included), and ELUC was 1.1 ± 0.7 GtC yr−1, for a total anthropogenic CO2 emission (including the cement carbonation sink) of 10.9 ± 0.8 GtC yr−1 (40.0 ± 2.9 GtCO2). Also, for 2021, GATM was 5.2 ± 0.2 GtC yr−1 (2.5 ± 0.1 ppm yr−1), SOCEAN was 2.9 ± 0.4 GtC yr−1, and SLAND was 3.5 ± 0.9 GtC yr−1, with a BIM of −0.6 GtC yr−1 (i.e. the total estimated sources were too low or sinks were too high). The global atmospheric CO2 concentration averaged over 2021 reached 414.71 ± 0.1 ppm. Preliminary data for 2022 suggest an increase in EFOS relative to 2021 of +1.0 % (0.1 % to 1.9 %) globally and atmospheric CO2 concentration reaching 417.2 ppm, more than 50 % above pre-industrial levels (around 278 ppm). Overall, the mean and trend in the components of the global carbon budget are consistently estimated over the period 1959–2021, 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 change emissions, (2) a low agreement between the different methods on the magnitude of the land CO2 flux in the northern extratropics, 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 data sets used in this new global carbon budget and the progress in understanding of the global carbon cycle compared with previous publications of this data set. The data presented in this work are available at https://doi.org/10.18160/GCP-2022 (Friedlingstein et al., 2022b). |
| Audience | PUBLIC Academic |
| Author | Alin, Simone R Falk, Stefanie Gehlen, Marion Sitch, Stephen Alkama, Ramdane Chevallier, Frédéric O'Sullivan, Michael Andrew, Robbie M Gregor, Luke Bittig, Henry C Chini, Louise P Quéré, Corinne Le Poulter, Benjamin Peters, Wouter Olsen, Are Bopp, Laurent Gkritzalis, Thanos Ciais, Philippe Bates, Nicholas R Jones, Matthew W Jackson, Robert B Arora, Vivek K Luijkx, Ingrid T Peters, Glen P Hauck, Judith Pongratz, Julia Bellouin, Nicolas Schwingshackl, Clemens Canadell, Josep G Evans, Wiley Feely, Richard A Cronin, Margot Gasser, Thomas Friedlingstein, Pierre Arneth, Almut Becker, Meike |
| Author_xml | – sequence: 1 givenname: Pierre orcidid: 0000-0003-3309-4739 surname: Friedlingstein fullname: Friedlingstein, Pierre organization: University of Exeter – sequence: 2 givenname: Michael orcidid: 0000-0002-6278-3392 surname: O'Sullivan fullname: O'Sullivan, Michael organization: University of Exeter – sequence: 3 givenname: Matthew W surname: Jones fullname: Jones, Matthew W organization: University of East Anglia – sequence: 4 givenname: Robbie M orcidid: 0000-0001-8590-6431 surname: Andrew fullname: Andrew, Robbie M organization: CICERO Center for International Climate Research – sequence: 5 givenname: Luke orcidid: 0000-0001-6071-1857 surname: Gregor fullname: Gregor, Luke organization: ETH Zurich – sequence: 6 givenname: Judith orcidid: 0000-0003-4723-9652 surname: Hauck fullname: Hauck, Judith organization: Alfred Wegener Institute for Polar and Marine Research – sequence: 7 givenname: Corinne Le orcidid: 0000-0003-2319-0452 surname: Quéré fullname: Quéré, Corinne Le organization: University of East Anglia – sequence: 8 givenname: Ingrid T orcidid: 0000-0002-3990-6737 surname: Luijkx fullname: Luijkx, Ingrid T organization: Wageningen University & Research – sequence: 9 givenname: Are orcidid: 0000-0003-1696-9142 surname: Olsen fullname: Olsen, Are organization: University of Bergen – sequence: 10 givenname: Glen P orcidid: 0000-0001-7889-8568 surname: Peters fullname: Peters, Glen P organization: CICERO Center for International Climate Research – sequence: 11 givenname: Wouter orcidid: 0000-0001-8166-2070 surname: Peters fullname: Peters, Wouter organization: Wageningen University & Research – sequence: 12 givenname: Julia orcidid: 0000-0003-0372-3960 surname: Pongratz fullname: Pongratz, Julia organization: Max Planck Institute for Meteorology – sequence: 13 givenname: Clemens orcidid: 0000-0003-4048-3011 surname: Schwingshackl fullname: Schwingshackl, Clemens organization: Ludwig Maximilian University of Munich – sequence: 14 givenname: Stephen surname: Sitch fullname: Sitch, Stephen organization: University of Exeter – sequence: 15 givenname: Josep G orcidid: 0000-0002-8788-3218 surname: Canadell fullname: Canadell, Josep G organization: CSIRO Ocean and Atmosphere – sequence: 16 givenname: Philippe orcidid: 0000-0001-8560-4943 surname: Ciais fullname: Ciais, Philippe organization: Laboratoire des Sciences du Climat et de l'Environnement – sequence: 17 givenname: Robert B orcidid: 0000-0001-8846-7147 surname: Jackson fullname: Jackson, Robert B organization: Stanford University – sequence: 18 givenname: Simone R surname: Alin fullname: Alin, Simone R organization: Pacific Marine Environmental Laboratory – sequence: 19 givenname: Ramdane surname: Alkama fullname: Alkama, Ramdane organization: Joint Research Centre – sequence: 20 givenname: Almut orcidid: 0000-0001-6616-0822 surname: Arneth fullname: Arneth, Almut organization: Karlsruhe Institute of Technology – sequence: 21 givenname: Vivek K surname: Arora fullname: Arora, Vivek K organization: Environment and Climate Change Canada – sequence: 22 givenname: Nicholas R surname: Bates fullname: Bates, Nicholas R organization: Bermuda Institute of Ocean Sciences – sequence: 23 givenname: Meike orcidid: 0000-0001-7650-0923 surname: Becker fullname: Becker, Meike organization: University of Bergen – sequence: 24 givenname: Nicolas orcidid: 0000-0003-2109-9559 surname: Bellouin fullname: Bellouin, Nicolas organization: University of Reading – sequence: 25 givenname: Henry C orcidid: 0000-0002-8621-3095 surname: Bittig fullname: Bittig, Henry C organization: Leibniz Institute for Baltic Sea Research – sequence: 26 givenname: Laurent orcidid: 0000-0003-4732-4953 surname: Bopp fullname: Bopp, Laurent organization: Laboratoire de Météorologie Dynamique – sequence: 27 givenname: Frédéric orcidid: 0000-0002-4327-3813 surname: Chevallier fullname: Chevallier, Frédéric organization: Laboratoire des Sciences du Climat et de l'Environnement – sequence: 28 givenname: Louise P orcidid: 0000-0002-9070-3505 surname: Chini fullname: Chini, Louise P organization: University of Maryland, College Park – sequence: 29 givenname: Margot surname: Cronin fullname: Cronin, Margot organization: Marine Institute – sequence: 30 givenname: Wiley orcidid: 0000-0002-5450-0903 surname: Evans fullname: Evans, Wiley organization: Hakai Institute – sequence: 31 givenname: Stefanie orcidid: 0000-0002-4552-5455 surname: Falk fullname: Falk, Stefanie organization: Ludwig Maximilian University of Munich – sequence: 32 givenname: Richard A surname: Feely fullname: Feely, Richard A organization: Pacific Marine Environmental Laboratory – sequence: 33 givenname: Thomas orcidid: 0000-0003-4882-2647 surname: Gasser fullname: Gasser, Thomas organization: International Institute for Applied Systems Analysis – sequence: 34 givenname: Marion orcidid: 0000-0002-9688-0692 surname: Gehlen fullname: Gehlen, Marion organization: Laboratoire des Sciences du Climat et de l'Environnement – sequence: 35 givenname: Thanos surname: Gkritzalis fullname: Gkritzalis, Thanos organization: Flanders Marine Institute – sequence: 36 givenname: Benjamin orcidid: 0000-0002-9493-8600 surname: Poulter fullname: Poulter, Benjamin organization: Goddard Space Flight Center |
| BackLink | https://cnrs.hal.science/hal-03863123$$DView record in HAL https://www.osti.gov/biblio/1897754$$D View this record in Osti.gov |
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| PublicationDate | 2022-11-11 |
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| PublicationTitle | Earth system science data |
| PublicationYear | 2022 |
| Publisher | Copernicus.org (Germany) Copernicus GmbH Copernicus Publications |
| Publisher_xml | – sequence: 0 name: Copernicus Publications – name: Copernicus.org (Germany) – name: Copernicus GmbH – name: Copernicus Publications |
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| Snippet | Accurate assessment of anthropogenic carbon dioxide (CO2) emissions and their redistribution among the atmosphere, ocean, and terrestrial biosphere in a... Accurate assessment of anthropogenic carbon dioxide (CO.sub.2) emissions and their redistribution among the atmosphere, ocean, and terrestrial biosphere in a... |
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| SubjectTerms | Anthropogenic factors Atmosphere Atmospheric models Biogeochemistry Biosphere Budget Carbon Carbon budget Carbon cycle Carbon cycle (Biogeochemistry) Carbon dioxide Carbon dioxide emissions Carbonation Cement Chemical oceanography Climate change Climate policy Components Concrete Datasets Deforestation Documents Earth Resources and Remote Sensing Emissions ENVIRONMENTAL SCIENCES Estimates Fossil fuels Fossils Future climates Global Changes Global temperature changes Growth rate Land use Ocean models Oceans Statistical methods Trends Uncertainty Vegetation |
| Title | Global Carbon Budget 2022 |
| URI | https://ntrs.nasa.gov/citations/20230013723 https://www.proquest.com/docview/2753485505 https://cnrs.hal.science/hal-03863123 https://www.osti.gov/biblio/1897754 |
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