Fifty years of carbon dioxide (CO2) measurements in the background atmosphere of SE Australia
P. Fraser, R. Langenfelds, N. Derek, P. Krummel, Z. Loh, CSIRO Oceans and Atmosphere, Aspendale, Victoria
March 2022
In a landmark paper in Nature in 19731, CSIRO scientists John Garratt and Graeme Pearman announced the first results of a new CSIRO program to measure atmosphere-ocean carbon dioxide (CO2) fluxes in the Southern Hemisphere:
‘An atmospheric carbon dioxide monitoring program, based on the collection of discrete air samples from aircraft, was initiated in early 1972 at the CSIRO Division of Atmospheric Physics in Australia’.
Thus began CSIRO’s innovative and globally important greenhouse gas (GHG) research program2, measuring (Figure 1) and modelling CO2 in the mid- to high latitudes of the Southern Hemisphere. The program subsequently expanded to include a range of non-CO2 GHGs, for example chlorofluorocarbons – CFCs from around 1975.
This CSIRO led work helped support the establishment in 1976 of the iconic Kennaook Cape Grim baseline station4, in partnership with the Australian Bureau of Meteorology.
CSIRO’s CO2 and non-CO2 GHG data, their interpretation and modelling, have been integral to every international assessment of climate change science and ozone depletion science (of which there have been 6 since 1990 and 12 since 1985, respectively).
The first air samples in this program were collected on Tuesday 21 March 1972 at 4.0 km over the middle of Bass Strait, with a recorded CO2 concentration of 327 ppm (parts per million molar). 50 years later, the mean baseline CO2 concentration (413 ppm) recorded at Kennaook / Cape Grim in early 2022 was 413 ppm. That is 26‑27% higher than when the program commenced, and 48% higher than CSIRO’s records of pre-industrial (circa 1750) CO2 concentrations, based on air extracted from Antarctic ice-cores (typically quoted as 278 ppm).
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Preparing flasks for sampling on board a 727 aircraft, 1972
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Analysing flasks for CO2 concentration, 1970s

Kennaook (Cape Grim) Baseline Air Station, 2021
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Original pump unit from the 1970s

Some of the original CO2 measurement group along with the current and future CO2 researchers
Back row (L2R): Paul Fraser, Colin Allison, Graeme Pearman, John Garratt, Roger Francey, David Thornton, Ray Langenfelds, David Etheridge
Front row (L2R): Zoe Loh, Paul Krummel, Nada Derek, Ann Stavert and son.
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Part of the current greenhouse measurement suite at Kennaook (Cape Grim), Tasmania
1Garratt, J. R. and G. I. Pearman, Large-scale CO2 fluxes in the Southern Hemisphere troposphere, Nature, 242, 54-56, 1973, doi.org/10.1038/physci242054a0, 26 March 1973.
2Pearman, G. I., J. R. Garratt and P. J. Fraser, CSIRO high-precision measurements of atmospheric CO2 concentration in Australia. Part 1: Initial motivation, techniques and aircraft sampling, Historical Records of Australian Science, 28 (2) 111 – 125, 2017, doi.10.1071/HR17014.
3Fraser, P. J., G. I. Pearman and N. Derek, CSIRO non-carbon dioxide greenhouse gas research. Part 1: 1975-1990, Historical Records of Australian Science, 29 (1), 1-13, 2018, doi.10.1071/HR17016.
4Pearman, G. I., P. J. Fraser and J. R. Garratt, CSIRO high-precision measurements of atmospheric CO2 concentration in Australia. Part 2: Cape Grim, surface CO2 measurements and carbon cycle modelling, Historical Records of Australian Science, 28 (2,) 126 – 139, 2017, doi.10.1071/HR17015.