Global Carbon Budget 2021

Medientyp: E-Artikel

Titel: Global Carbon Budget 2021

Beteiligte: Friedlingstein, Pierre; Jones, Matthew W.; O'Sullivan, Michael; Andrew, Robbie M.; Bakker, Dorothee C. E.; Hauck, Judith; Le Quéré, Corinne; Peters, Glen P.; Peters, Wouter; Pongratz, Julia; Sitch, Stephen; Canadell, Josep G.; Ciais, Philippe; Jackson, Rob B.; Alin, Simone R.; Anthoni, Peter; Bates, Nicholas R.; Becker, Meike; Bellouin, Nicolas; Bopp, Laurent; Chau, Thi Tuyet Trang; Chevallier, Frédéric; Chini, Louise P.; Cronin, Margot; [...]

Erschienen: Copernicus GmbH, 2022

Umfang: 1917-2005

Sprache: Englisch

DOI: 10.5194/essd-14-1917-2022

ISSN: 1866-3516

Schlagwörter: General Earth and Planetary Sciences

Zusammenfassung: 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).

Beschreibung: 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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