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CO₂ and Greenhouse Gas Emissions

Human emissions of greenhouse gases are the primary driver of climate change today.1

CO2 and other greenhouse gases like methane and nitrous oxide are emitted when we burn fossil fuels, produce materials such as steel, cement, and plastics, and grow the food we eat. If we want to reduce these emissions, we need to transform our energy systems, industries, and food systems.

At the same time, we need to tackle energy poverty, low standards of living, and poor nutrition, which all remain enormous problems for billions of people.

Technological advances could allow us to do both. The prices of solar, wind, and batteries have plummeted in recent decades, increasingly undercutting the cost of fossil fuel alternatives. Further progress could allow us to provide cheap, clean energy for everyone. Political change is essential to create a system that supports rapid decarbonization.

Emissions are still rising in many parts of the world. However, several countries have managed to cut their emissions in recent decades. With affordable low-carbon technologies, other countries can increase their living standards without the high-carbon pathway that rich countries followed in the past.

On this page, you can find our data, visualizations, and writing on CO2 and other greenhouse gas emissions.

Key Insights on CO₂ and Greenhouse Gas Emissions

Human greenhouse gas emissions have increased global average temperatures

Human emissions of carbon dioxide and other greenhouse gases are the primary drivers of the global rise in temperatures.1 This link between global temperatures and greenhouse gas concentrations – especially CO2 – has been true throughout Earth’s history.2

In the chart, we see the global average temperature relative to a baseline, which is the average between 1961 and 1990. Average temperatures have risen by over 0.8°C since then.

You can also see that temperatures in 1850 were around 0.4°C cooler than the baseline, giving us a total temperature rise of about 1.2°C compared to pre-industrial times.

This warming has not been equally distributed across the world. The Northern Hemisphere has warmed more than the Southern Hemisphere. And warming has been especially strong at the poles. In some regions, temperatures have risen by more than 5°C. You can see this distribution in maps published by Berkeley Earth.

Human emissions have been the main driver of this change. Aerosols have played a slight cooling role in global climate, and natural variability has played a minor role. This article from Carbon Brief explains this very well, with interactive graphics showing the relative contributions of different factors on the climate.

What you should know about this data
  • This data comes from the United Kingdom’s Met Office and combines air and sea surface temperatures in the Northern and Southern Hemispheres. It is called the “HadCRUT” (Hadley Centre/Climatic Research Unit Temperature) dataset.3
  • It measures temperature anomalies across the world at high resolutions.
  • There is very strong agreement in temperature trends across the large global datasets measured and produced by other leading institutions.

Global emissions have increased rapidly over the last 50 years and have not yet peaked

If we want to stabilize (or even reduce) concentrations of CO2 in the atmosphere, the world needs to reach net-zero emissions. This means our net carbon contributions to the atmosphere are zero: any remaining emissions are offset by carbon sinks. This requires significant reductions in emissions.

However, emissions from fossil fuels have not yet peaked.

In the chart, you can see global CO2 emissions since 1750, broken down by world region. Emissions have increased rapidly over the last half-century.

While this growth rate has slowed recently, fossil emissions are still rising.

What you should know about this data
  • CO2 emissions are for fossil fuel and industrial emissions only. Land use changes are not included but can be viewed in our data explorer.
  • Emissions are allocated to countries based on production – they do not adjust for trade. Trade-adjusted emissions can be found in our CO2 Data Explorer.

Current climate policies will reduce emissions, but not enough to keep temperature rise below 2°C

Current policies to reduce, or at least slow down, the growth of CO2 emissions have already averted some future warming compared to a world without these policies.

As we see in the chart, climate and energy policies – which include adopted and implemented policies (such as legislative decisions and executive orders) would reduce warming relative to a world with no climate policies.

This chart maps out future greenhouse gas emissions scenarios under a range of assumptions: if no climate policies were implemented; if current policies continued; if all countries achieved their current future pledges for emissions reductions; and the necessary pathways compatible with limiting warming to 1.5°C or 2°C of warming this century.4

Current policies have us on track for around 2.7°C by 2100.

And if countries achieved their current pledges, this could be reduced to 2.1°C.

But if we aim to limit warming to “well below 2°C” – as is laid out in the Paris Agreement – currently policies have us far off track. To achieve this goal, countries need to increase the ambition of these commitments and bring their policies in line with them.

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There are large differences in emissions across the world

There is no single metric that captures the distribution of CO2 emissions across the world, today or in the past.

We can compare the total emissions of countries every year. But this fails to take population size into account; you’d expect a country with more people to have higher emissions. Even then, comparisons of total or per capita emissions today don’t capture historical contributions. Some countries that now have relatively low emissions have had high emissions for centuries.

These metrics tell us different things. We make all of them available by country in our data explorer.

In the chart, we see one metric to compare across the world: emissions per person. There are massive differences in emissions across the globe. Some of the wealthiest countries emit 100 times more per person than the poorest.

Read more:

There are many ways to measure countries’ contributions to climate change. What do they tell us?

Many countries have reduced their CO₂ emissions

Global emissions are still rising, but many countries have managed to reduce their emissions in recent decades.

Domestic emissions in the UK have roughly halved since 1970. Emissions in the European Union have fallen by more than one-quarter.

Part of this is because many rich countries have ‘offshored’ some of their emissions by importing CO2-intensive goods manufactured elsewhere – but we still see a significant decline in emissions after adjusting for trade. Consumption-based CO2 emissions have declined very substantially in many countries.

Many of these countries have grown their economies at the same time: GDP per capita has increased while consumption-based emissions have fallen. The chart shows the data for various countries that have achieved this decoupling.

Read more:

Which countries are net importers and exports of emissions? How much CO2 is ‘offshored’?

It is possible to reduce emissions while growing the economy. But this decoupling needs to happen faster.

What you should know about this data
  • Consumption-based emissions adjust for imported and exported emissions based on global trade flows. These emissions are domestic emissions plus imported emissions minus exported emissions.
  • CO2 emissions are for fossil fuel and industrial emissions only. Land use changes are not included but can be viewed in our data explorer.
Grid of charts showing the percentage increase in GDP per capita and the percentage decrease in CO2 emissions per capita, for many countries.

Explore Data on CO2 and Greenhouse Gas Emissions

Research & Writing

Interactive Charts on CO₂ and Greenhouse Gas Emissions

Endnotes

  1. IPCC, 2021: Climate Change 2021: The Physical Science Basis. Contribution of Working Group I to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change [Masson-Delmotte, V., P. Zhai, A. Pirani, S.L. Connors, C. Péan, S. Berger, N. Caud, Y. Chen, L. Goldfarb, M.I. Gomis, M. Huang, K. Leitzell, E. Lonnoy, J.B.R. Matthews, T.K. Maycock, T. Waterfield, O. Yelekçi, R. Yu, and B. Zhou (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, In press, doi:10.1017/9781009157896.

  2. Lacis, A. A., Schmidt, G. A., Rind, D., & Ruedy, R. A. (2010). Atmospheric CO₂: Principal control knob governing Earth’s temperature. Science, 330(6002), 356-359.

  3. Morice, C.P., J.J. Kennedy, N.A. Rayner, J.P. Winn, E. Hogan, R.E. Killick, R.J.H. Dunn, T.J. Osborn, P.D. Jones and I.R. Simpson (in press) An updated assessment of near-surface temperature change from 1850: the HadCRUT5 dataset. Journal of Geophysical Research (Atmospheres) doi:10.1029/2019JD032361 (supporting information).

  4. The underlying data for this chart is sourced from the Climate Action Tracker – based on policies and pledges as of April 2022.

Cite this work

Our articles and data visualizations rely on work from many different people and organizations. When citing this topic page, please also cite the underlying data sources. This topic page can be cited as:

Hannah Ritchie, Pablo Rosado and Max Roser (2023) - “CO₂ and Greenhouse Gas Emissions” Published online at OurWorldinData.org. Retrieved from: 'https://ourworldindata.org/co2-and-greenhouse-gas-emissions' [Online Resource]

BibTeX citation

@article{owid-co2-and-greenhouse-gas-emissions,
    author = {Hannah Ritchie and Pablo Rosado and Max Roser},
    title = {CO₂ and Greenhouse Gas Emissions},
    journal = {Our World in Data},
    year = {2023},
    note = {https://ourworldindata.org/co2-and-greenhouse-gas-emissions}
}
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