TY - JOUR
T1 - Global Carbon Budget 2019
AU - Friedlingstein, Pierre
AU - Jones, Matthew W.
AU - O'Sullivan, Michael
AU - Andrew, Robbie M.
AU - Hauck, Judith
AU - Peters, Glen P.
AU - Peters, Wouter
AU - Pongratz, Julia
AU - Sitch, Stephen
AU - Le Quere, Corinne
AU - Bakker, Dorothee C. E.
AU - Canadell, Josep G.
AU - Ciais, Philippe
AU - Jackson, Robert B.
AU - Anthoni, Peter
AU - Barbero, Leticia
AU - Bastos, Ana
AU - Bastrikov, Vladislav
AU - Becker, Meike
AU - Bopp, Laurent
AU - Buitenhuis, Erik
AU - Chandra, Naveen
AU - Chevallier, Frederic
AU - Chini, Louise P.
AU - Currie, Kim I.
AU - Feely, Richard A.
AU - Gehlen, Marion
AU - Gilfillan, Dennis
AU - Gkritzalis, Thanos
AU - Goll, Daniel S.
AU - Gruber, Nicolas
AU - Gutekunst, Soeren
AU - Harris, Ian
AU - Haverd, Vanessa
AU - Houghton, Richard A.
AU - Hurtt, George
AU - Ilyina, Tatiana
AU - Jain, Atul K.
AU - Joetzjer, Emilie
AU - Kaplan, Jed O.
AU - Kato, Etsushi
AU - Goldewijk, Kees Klein
AU - Korsbakken, Jan Ivar
AU - Landschuetzer, Peter
AU - Lauvset, Siv K.
AU - Lefevre, Nathalie
AU - Lenton, Andrew
AU - Lienert, Sebastian
AU - Lombardozzi, Danica
AU - Marland, Gregg
AU - McGuire, Patrick C.
AU - Melton, Joe R.
AU - Metzl, Nicolas
AU - Munro, David R.
AU - Nabel, Julia E. M. S.
AU - Nakaoka, Shin-Ichiro
AU - Neill, Craig
AU - Omar, Abdirahman M.
AU - Ono, Tsuneo
AU - Peregon, Anna
AU - Pierrot, Denis
AU - Poulter, Benjamin
AU - Rehder, Gregor
AU - Resplandy, Laure
AU - Robertson, Eddy
AU - Rodenbeck, Christian
AU - Seferian, Roland
AU - Schwinger, Joerg
AU - Smith, Naomi
AU - Tans, Pieter P.
AU - Tian, Hanqin
AU - Tilbrook, Bronte
AU - Tubiello, Francesco N.
AU - van der Werf, Guido R.
AU - Wiltshire, Andrew J.
AU - Zaehle, Sonke
PY - 2019/12/4
Y1 - 2019/12/4
N2 - 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. Fossil CO2 emissions (E-FF) 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) and terrestrial CO2 sink (S-LAND) are estimated with global process models constrained by observations. 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 understanding of the contemporary carbon cycle. All uncertainties are reported as +/- 1 sigma. For the last decade available (2009-2018), E-FF was 9.5 +/- 0.5 GtC yr 1, E-LUC 1.5 +/- 0.7 GtC yr 1, G(ATM) 4.9 +/- 0.02 GtC yr(-1) (2.3 +/- 0.01 ppm yr(-1)), S-OCEAN 2.5 +/- 0.6 GtC yr(-1), and S-LAND 3.2 +/- 0.6 GtC yr(-1), with a budget imbalance B-IM of 0.4 GtC yr(-1) indicating overestimated emissions and/or underestimated sinks. For the year 2018 alone, the growth in E-FF was about 2.1% and fossil emissions increased to 10.0 +/- 0.5 GtC yr 1, reaching 10 GtC yr(-1) for the first time in history, E-LUC was 1.5 +/- 0.7 GtC yr(-1), for total anthropogenic CO2 emissions of 11.5 +/- 0.9 GtC yr(-1) (42.5 +/- 3.3 GtCO(2)). Also for 2018, G(ATM) was 5.1 +/- 0.2 GtC yr(-1) (2.4 +/- 0.1 ppm yr(-1)), S-OCEAN was 2.6 +/- 0.6 GtC yr(-1), and S-LAND was 3.5 +/- 0.7 GtC yr(-1), with a B-IM of 0.3 GtC. The global atmospheric CO2 concentration reached 407.38 +/- 0.1 ppm averaged over 2018. For 2019, preliminary data for the first 6-10 months indicate a reduced growth in E-FF of +0.6% (range of -0.2% to 1.5 %) based on national emissions projections for China, the USA, the EU, and India and projections of gross domestic product corrected for recent changes in the carbon intensity of the economy for the rest of the world. Overall, the mean and trend in the five components of the global carbon budget are consistently estimated over the period 1959-2018, but discrepancies of up to 1 GtC yr(-1) persist for the representation of semi-decadal variability in CO2 fluxes.A detailed comparison among individual estimates and the introduction of a broad range of observations shows (1) no consensus in the mean and trend in land use change emissions over the last decade, (2) a persistent low agreement between the different methods on the magnitude of the land CO2 flux in the northern extra-tropics, and (3) an apparent underestimation of the CO2 variability by ocean models outside the tropics. 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 (Le Quere et al., 2018a, b, 2016, 2015a, b, 2014, 2013).
AB - 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. Fossil CO2 emissions (E-FF) 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) and terrestrial CO2 sink (S-LAND) are estimated with global process models constrained by observations. 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 understanding of the contemporary carbon cycle. All uncertainties are reported as +/- 1 sigma. For the last decade available (2009-2018), E-FF was 9.5 +/- 0.5 GtC yr 1, E-LUC 1.5 +/- 0.7 GtC yr 1, G(ATM) 4.9 +/- 0.02 GtC yr(-1) (2.3 +/- 0.01 ppm yr(-1)), S-OCEAN 2.5 +/- 0.6 GtC yr(-1), and S-LAND 3.2 +/- 0.6 GtC yr(-1), with a budget imbalance B-IM of 0.4 GtC yr(-1) indicating overestimated emissions and/or underestimated sinks. For the year 2018 alone, the growth in E-FF was about 2.1% and fossil emissions increased to 10.0 +/- 0.5 GtC yr 1, reaching 10 GtC yr(-1) for the first time in history, E-LUC was 1.5 +/- 0.7 GtC yr(-1), for total anthropogenic CO2 emissions of 11.5 +/- 0.9 GtC yr(-1) (42.5 +/- 3.3 GtCO(2)). Also for 2018, G(ATM) was 5.1 +/- 0.2 GtC yr(-1) (2.4 +/- 0.1 ppm yr(-1)), S-OCEAN was 2.6 +/- 0.6 GtC yr(-1), and S-LAND was 3.5 +/- 0.7 GtC yr(-1), with a B-IM of 0.3 GtC. The global atmospheric CO2 concentration reached 407.38 +/- 0.1 ppm averaged over 2018. For 2019, preliminary data for the first 6-10 months indicate a reduced growth in E-FF of +0.6% (range of -0.2% to 1.5 %) based on national emissions projections for China, the USA, the EU, and India and projections of gross domestic product corrected for recent changes in the carbon intensity of the economy for the rest of the world. Overall, the mean and trend in the five components of the global carbon budget are consistently estimated over the period 1959-2018, but discrepancies of up to 1 GtC yr(-1) persist for the representation of semi-decadal variability in CO2 fluxes.A detailed comparison among individual estimates and the introduction of a broad range of observations shows (1) no consensus in the mean and trend in land use change emissions over the last decade, (2) a persistent low agreement between the different methods on the magnitude of the land CO2 flux in the northern extra-tropics, and (3) an apparent underestimation of the CO2 variability by ocean models outside the tropics. 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 (Le Quere et al., 2018a, b, 2016, 2015a, b, 2014, 2013).
KW - LAND-COVER CHANGE
KW - EARTH SYSTEM MODEL
KW - ENVIRONMENT SIMULATOR JULES
KW - OCEAN BIOGEOCHEMICAL MODEL
KW - ANTHROPOGENIC CO2 UPTAKE
KW - LEAF-AREA INDEX
KW - ATMOSPHERIC CO2
KW - SURFACE-OCEAN
KW - FOSSIL-FUEL
KW - DIOXIDE EMISSIONS
U2 - 10.5194/essd-11-1783-2019
DO - 10.5194/essd-11-1783-2019
M3 - Article
SN - 1866-3508
VL - 11
SP - 1783
EP - 1838
JO - Earth System Science Data
JF - Earth System Science Data
IS - 4
ER -