What is the Yearly Average Atmospheric CO₂?

This is the average amount of CO2 that is in the atmosphere in a given year. The yearly average highlights the long-term trends of atmospheric CO₂ and allows us to see modern day levels compared to pre-industrial levels, even as far back as the last 800,000 years. This is critical because the amount of CO₂ in the atmosphere is directly related to the warming of the Earth. The warming impact due to atmospheric CO₂ can be seen in the Monthly Greenhouse Gases Impact on Energy Balance.

Units and measures

The primary unit here is parts per million (ppm), which describes the concentration of atmospheric CO₂ per year. The secondary unit here is gigatonnes, which describes the weight of atmospheric CO₂ per year. We show this to be able to relate to emissions, which are commonly expressed in gigatonnes.

Insights from this chart

In 60 years the CO₂ concentration has steadily risen from just over 300 ppm to more than 400 ppm. To get a feeling for the natural concentrations of CO₂, we can compare this to historical values.

When we look at the last 1,000 years, we can clearly see that the CO₂ level started rising at the end of the 18th century, coinciding with the industrial revolution.

Throughout the last glacial period, roughly 100,000 to 12,000 years ago, we can see a drastic variation in CO₂ levels. This was also a drastic period! Ice sheets reached the northern parts of the US, the UK, Germany and Northeast Siberia. There were sea-level changes up to 120 meters. However, the changes in CO₂ levels were smaller and much slower compared to what we have been experiencing over the last 200 years.

The last 800,000 years offer some perspective on the CO₂ levels during the recurring glacial periods and the unusually high CO₂ level of our time. The current level of over 400 ppm was unheard of in the past, which saw values between 180 ppm and 300 ppm.

About the data

The data are from the Global Carbon Budget 2022 and two subgroups of NOAA, the Global Monitoring Laboratory for recent data and the National Centers for Environmental Information for paleoclimatology data.

The Global Monitoring Laboratory has a global network of air sampling sites where they measure CO₂. They have an annual mean dataset starting in 1980. For the years between 1959 and today that are unavailable, the atmospheric increase values are used to calculate an estimate for the annual means.

The Global Carbon Budget 2023 provides yearly atmospheric increase values going back to 1750, which are used to estimate the yearly atmospheric CO₂ between 1750 and 1959.

National Centers for Environmental Information holds datasets that contain reconstructions of historic CO₂ levels going back 800,000 years based on Antarctic ice cores.

Data sources

Globally averaged marine surface annual mean rates data NOAA's Global Monitoring Laboratory
Credits: Ed Dlugokencky and Pieter Tans, NOAA/GML (gml.noaa.gov/ccgg/trends/)Update cycle: yearlyDelay: ~ 3 months

Globally averaged marine surface annual mean growth rates data NOAA's Global Monitoring Laboratory
Credits: Ed Dlugokencky and Pieter Tans, NOAA/GML (gml.noaa.gov/ccgg/trends/)Update cycle: monthlyDelay: ~ 3 months

Globally averaged marine surface monthly mean data NOAA's Global Monitoring Laboratory
Credits: Ed Dlugokencky and Pieter Tans, NOAA/GML (gml.noaa.gov/ccgg/trends/)Update cycle: monthlyDelay: ~ 3 months

Estimated Global Trend daily values NOAA's Global Monitoring Laboratory
Credits: Ed Dlugokencky and Pieter Tans, NOAA/GML (gml.noaa.gov/ccgg/trends/)Update cycle: dailyDelay: ~ 2 days

Antarctic Ice Core Revised Composite and Individual Core CO₂ Data NOAA's National Centers for Environmental Information
Credits: Bernhard Bereiter, Sarah Eggleston, Jochen Schmitt, Christoph Nehrbass-Ahles, Thomas F. Stocker, Hubertus Fischer, Sepp Kipfstuhl and Jerome Chappellaz. 2015. Revision of the EPICA Dome C CO₂ record from 800 to 600 kyr before present. Geophysical Research Letters. . doi: 10.1002/2014GL061957

Global Carbon Budget 2023 Global Carbon Budget
Credits: Friedlingstein et al., 2023b, ESSD, full reference below **Update cycle: yearlyDelay: ~ 10 months after end of a year. Current year values estimates published in November.Reference: ** Friedlingstein, P., O'Sullivan, M., Jones, M. W., Andrew, R. M., Bakker, D. C. E., Hauck, J., Landschützer, P., Le Quéré, C., Luijkx, I. T., Peters, G. P., Peters, W., Pongratz, J., Schwingshackl, C., Sitch, S., Canadell, J. G., Ciais, P., Jackson, R. B., Alin, S. R., Anthoni, P., Barbero, L., Bates, N. R., Becker, M., Bellouin, N., Decharme, B., Bopp, L., Brasika, I. B. M., Cadule, P., Chamberlain, M. A., Chandra, N., Chau, T.-T.-T., Chevallier, F., Chini, L. P., Cronin, M., Dou, X., Enyo, K., Evans, W., Falk, S., Feely, R. A., Feng, L., Ford, D. J., Gasser, T., Ghattas, J., Gkritzalis, T., Grassi, G., Gregor, L., Gruber, N., Gürses, Ö., Harris, I., Hefner, M., Heinke, J., Houghton, R. A., Hurtt, G. C., Iida, Y., Ilyina, T., Jacobson, A. R., Jain, A., Jarníková, T., Jersild, A., Jiang, F., Jin, Z., Joos, F., Kato, E., Keeling, R. F., Kennedy, D., Klein Goldewijk, K., Knauer, J., Korsbakken, J. I., Körtzinger, A., Lan, X., Lefèvre, N., Li, H., Liu, J., Liu, Z., Ma, L., Marland, G., Mayot, N., McGuire, P. C., McKinley, G. A., Meyer, G., Morgan, E. J., Munro, D. R., Nakaoka, S.-I., Niwa, Y., O'Brien, K. M., Olsen, A., Omar, A. M., Ono, T., Paulsen, M., Pierrot, D., Pocock, K., Poulter, B., Powis, C. M., Rehder, G., Resplandy, L., Robertson, E., Rödenbeck, C., Rosan, T. M., Schwinger, J., Séférian, R., Smallman, T. L., Smith, S. M., Sospedra-Alfonso, R., Sun, Q., Sutton, A. J., Sweeney, C., Takao, S., Tans, P. P., Tian, H., Tilbrook, B., Tsujino, H., Tubiello, F., van der Werf, G. R., van Ooijen, E., Wanninkhof, R., Watanabe, M., Wimart-Rousseau, C., Yang, D., Yang, X., Yuan, W., Yue, X., Zaehle, S., Zeng, J., and Zheng, B.: Global Carbon Budget 2023, Earth Syst. Sci. Data, 15, 5301–5369, https://doi.org/10.5194/essd-15-5301-2023, 2023.