Authors
Corinne Le Quéré, Robbie M Andrew, Pierre Friedlingstein, Stephen Sitch, Julia Pongratz, Andrew C Manning, Jan Ivar Korsbakken, Glen P Peters, Josep G Canadell, Robert B Jackson, Thomas A Boden, Pieter P Tans, Oliver D Andrews, Vivek K Arora, Dorothee CE Bakker, Leticia Barbero, Meike Becker, Richard A Betts, Laurent Bopp, Frédéric Chevallier, Louise P Chini, Philippe Ciais, Catherine E Cosca, Jessica Cross, Kim Currie, Thomas Gasser, Ian Harris, Judith Hauck, Vanessa Haverd, Richard A Houghton, Christopher W Hunt, George Hurtt, Tatiana Ilyina, Atul K Jain, Etsushi Kato, Markus Kautz, Ralph F Keeling, Kees Klein Goldewijk, Arne Körtzinger, Peter Landschützer, Nathalie Lefèvre, Andrew Lenton, Sebastian Lienert, Ivan Lima, Danica Lombardozzi, Nicolas Metzl, Frank Millero, Pedro Monteiro, David R Munro, Julia EMS Nabel, Shin-ichiro Nakaoka, Yukihiro Nojiri, X Antonio Padin, Anna Peregon, Benjamin Pfeil, Denis Pierrot, Benjamin Poulter, Gregor Rehder, Janet Reimer, Christian Rödenbeck, Jörg Schwinger, Roland Séférian, Ingunn Skjelvan, Benjamin D Stocker, Hanqin Tian, Bronte Tilbrook, Francesco N Tubiello, Ingrid T van Der Laan-Luijkx, Guido R van Der Werf, Steven Van Heuven, Nicolas Viovy, Nicolas Vuichard, Anthony P Walker, Andrew J Watson, Andrew J Wiltshire, Sönke Zaehle, Dan Zhu
Publication date
2018/3/12
Journal
Earth System Science Data
Volume
10
Issue
1
Pages
405-448
Publisher
Copernicus GmbH
Description
Accurate assessment of anthropogenic carbon dioxide (CO2) emissions and their redistribution among the atmosphere, ocean, and terrestrial biosphere – the global carbon budget – is important to better understand the global carbon cycle, support the development of climate policies, and project future climate change. Here we describe data sets and methodology to quantify the five major components of the global carbon budget and their uncertainties. CO2 emissions from fossil fuels and industry (EFF) are based on energy statistics and cement production data, respectively, while emissions from land-use change (ELUC), mainly deforestation, are based on land-cover change data and bookkeeping models. The global atmospheric CO2 concentration is measured directly and its rate of growth (GATM) is computed from the annual changes in concentration. The ocean CO2 sink (SOCEAN) and terrestrial CO2 sink (SLAND) are estimated with global process models constrained by observations. 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 last decade available (2007–2016), EFF was 9.4 ± 0.5 GtC yr−1, ELUC 1.3 ± 0.7 GtC yr−1, GATM 4.7 ± 0.1 GtC yr−1, SOCEAN 2.4 ± 0.5 GtC yr−1, and SLAND 3.0 ± 0.8 GtC yr−1, with a budget imbalance BIM of 0.6 GtC yr−1 indicating overestimated emissions and/or underestimated sinks. For year 2016 alone, the growth in EFF …
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Scholar articles
C Le Quéré, RM Andrew, P Friedlingstein, S Sitch… - Earth System Science Data, 2018