This is a breakdown by source of the yearly CO2 emissions from human activities and processes expressed in gigatonnes. It is critical to know and track the sources of human CO2 emissions in order to understand their individual impacts on climate change.
The sources of human CO2 emissions are
Fossil fuel CO2 emissions from the combustion of coal, oil and gas are emitted by processes in electricity generation, transport, industry, and the building sector. All processes can be linked to human activities. Examples include driving cars with combustion engines burning diesel or gas, or electric cars charged by electricity from a power plant that burns coal. To have a better picture of the human CO2 emissions linked to human activities, we are working on further trackable breakdowns.
Fossil CO2 emissions from other processes include sources like cement manufacturing and production of chemicals and fertilizers. Cement also has an absorption factor highlighted in the absorption breakdown chart.
Human civilization emits CO2 by changing and managing its land. Those emissions come, for example, from deforestation, logging, forest degradation, harvest activities and shifting agriculture cultivation. Land-use change also absorbs considerable amounts of CO2, which is shown in the absorption breakdown chart. Land-use change emits more than it absorbs, so the net effect is still emissions, but less than for coal, oil and gas.Wikipedia: Greenhouse Gas Emissions
CO2 emissions are expressed in the total weight in gigatonnes.Wikipedia: Gigatonne
Until the early 1900s, coal was the foremost fossil fuel, contributing to a steady rise in CO2 emissions. From 1910 to 1950, the use of coal didn’t really increase, with declines during the two world wars and the Great Depression. After 1950, coal use grew steadily once more until the 2000-2011 period, when the rapid development of China caused a major increase in CO2 emissions from coal combustion. The USA and Europe started reducing coal combustion around 2008. In the last ten years there has been no overall increase in coal use, but CO2 emissions from coal combustion are still very high.
After the Second World War came a quick growth in oil use that ended with the Arab oil embargo (1973) and the Iranian revolution (1979). Since then, the use of oil – and CO2 emissions from oil combustion – have grown steadily and are still very high.
Emissions from gas combustion have always been lower than those of coal and oil. They have been growing steadily since the 1960s and are still growing fast. Worldwide gas combustion produces almost the same amount of energy as oil and coal, but it emits less CO2, which is why many countries focus on first reducing coal and oil by switching to gas. Despite the lower emissions compared to other fossil fuels, gas combustion is still a major driver of climate change.
Land-use change emissions are very high and relatively steady. This chart shows the gross CO2 emissions due to anthropogenic land-use. Land-use change also absorbs significant amounts of CO2 from the atmosphere. The net effect is around 3 gigatonnes and is in a reducing trend. The significant peak of land CO2 emissions in 1997 is from Indonesian forest fires due to changes in land use.Global Carbon Project: Global Carbon Budget Presentation
The Global Carbon Project data for human emissions is the sum of the fossil CO2 emissions plus land-use change emissions. All values for 2022 are projections.
The fossil data is based on four main datasets containing global and national CO2 emissions. They estimate an uncertainty in global fossil CO2 emissions of ±5%.
Land-use change emissions are based on three bookkeeping models, and these models also estimate the land-use change absorption. There are large uncertainties in the land-use values before 1960.
Global Carbon Budget 2022Credits: Friedlingstein et al (2022) - full reference below**Update cycle: yearlyDelay: ~9 months after end of yearReference: ** Global Carbon Budget 2022, by Pierre Friedlingstein, Michael O'Sullivan, Matthew W. Jones, Robbie M. Andrew, Luke Gregor, Judith Hauck, Corinne Le Quéré, Ingrid T. Luijkx, Are Olsen, Glen P. Peters, Wouter Peters, Julia Pongratz, Clemens Schwingshackl, Stephen Sitch, Josep G. Canadell, Philippe Ciais, Robert B. Jackson, Simone R. Alin, Ramdane Alkama, Almut Arneth, Vivek K. Arora, Nicholas R. Bates, Meike Becker, Nicolas Bellouin, Henry C. Bittig, Laurent Bopp, Frédéric Chevallier, Louise P. Chini, Margot Cronin, Wiley Evans, Stefanie Falk, Richard A. Feely, Thomas Gasser, Marion Gehlen, Thanos Gkritzalis, Lucas Gloege, Giacomo Grassi, Nicolas Gruber, Özgür Gürses, Ian Harris, Matthew Hefner, Richard A. Houghton, George C. Hurtt, Yosuke Iida, Tatiana Ilyina, Atul K. Jain, Annika Jersild, Koji Kadono, Etsushi Kato, Daniel Kennedy, Kees Klein Goldewijk, Jürgen Knauer, Jan Ivar Korsbakken, Peter Landschützer, Nathalie Lefèvre, Keith Lindsay, Junjie Liu, Zhu Liu, Gregg Marland, Nicolas Mayot, Matthew J. McGrath, Nicolas Metzl, Natalie M. Monacci, David R. Munro, Shin-Ichiro Nakaoka, Yosuke Niwa, Kevin O'Brien, Tsuneo Ono, Paul I. Palmer, Naiqing Pan, Denis Pierrot, Katie Pocock, Benjamin Poulter, Laure Resplandy, Eddy Robertson, Christian Rödenbeck, Carmen Rodriguez, Thais M. Rosan, Jörg Schwinger, Roland Séférian, Jamie D. Shutler, Ingunn Skjelvan, Tobias Steinhoff, Qing Sun, Adrienne J. Sutton, Colm Sweeney, Shintaro Takao, Toste Tanhua, Pieter P. Tans, Xiangjun Tian, Hanqin Tian, Bronte Tilbrook, Hiroyuki Tsujino, Francesco Tubiello, Guido R. van der Werf, Anthony P. Walker, Rik Wanninkhof, Chris Whitehead, Anna Willstrand Wranne, Rebecca Wright,Wenping Yuan, Chao Yue, Xu Yue, Sönke Zaehle, Jiye Zeng, and Bo Zheng (2022), Earth System Science Data, 14, 4811–4900, 2022, DOI: 10.5194/essd-14-4811-2022.