Global Carbon Budget 2023

Media type: E-Article

Title: Global Carbon Budget 2023

Contributor: Friedlingstein, Pierre [Author]; O'Sullivan, Michael [Author]; Jones, Matthew W. [Author]; Andrew, Robbie M. [Author]; Bakker, Dorothee C. E. [Author]; Hauck, Judith [Author]; Landschützer, Peter [Author]; Le Quéré, Corinne [Author]; Luijkx, Ingrid T. [Author]; Peters, Glen P. [Author]; Peters, Wouter [Author]; Pongratz, Julia [Author]; Schwingshackl, Clemens [Author]; Sitch, Stephen [Author]; Canadell, Josep G. [Author]; Ciais, Philippe [Author]; Jackson, Robert B. [Author]; Alin, Simone R. [Author]; Anthoni, Peter [Author]; Barbero, Leticia [Author]; Bates, Nicholas R. [Author]; Becker, Meike [Author]; Bellouin, Nicolas [Author]; Decharme, Bertrand [Author]; [...]

Published: OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel), 2023-12-05

Language: English

DOI: https://doi.org/10.5194/essd-15-5301-2023

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Footnote: Diese Datenquelle enthält auch Bestandsnachweise, die nicht zu einem Volltext führen.

Description: 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 methodology to quantify the five major components of the global carbon budget and their uncertainties. Fossil CO2 emissions (E-FOS) are based on energy statistics and cement production data, while emissions from land-use change (E-LUC), 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 (G(ATM)) is computed from the annual changes in concentration. The ocean CO2 sink (S-OCEAN) is estimated with global ocean biogeochemistry models and observation-based fCO(2) products. The terrestrial CO2 sink (S-LAND) is estimated with dynamic global vegetation models. Additional lines of evidence on land and ocean sinks are provided by atmospheric inversions, atmospheric oxygen measurements, and Earth system models. The resulting carbon budget imbalance (B-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 incomplete understanding of the contemporary carbon cycle. All uncertainties are reported as +/- 1 sigma. For the year 2022, E-FOS increased by 0.9% relative to 2021, with fossil emissions at 9.9 +/- 0.5 GtC yr(-1) (10.2 +/- 0.5 GtC yr(-1) when the cement carbonation sink is not included), and E-LUC was 1.2 +/- 0.7 GtC yr(-1), for a total anthropogenic CO2 emission (including the cement carbonation sink) of 11.1 +/- 0.8 GtC yr(-1) (40.7 +/- 3.2 GtCO(2) yr(-1)). Also, for 2022, G(ATM) was 4.6 +/- 0.2 GtC yr(-1) (2.18 +/- 0.1 ppm yr(-1); ppm denotes parts per million), S-OCEAN was 2.8 +/- 0.4 GtC yr(-1), and S-LAND was 3.8 +/- 0.8 GtC yr(-1), with a ...

Access State: Open Access

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