Anthropogenic CO₂ increase is unprecedented
21 August 2020
Even in earlier warm periods there were pulse-like releases of CO₂ to the atmosphere. Today's anthropogenic CO₂ rise, however, is more than six times larger and almost ten times faster than previous jumps in the CO₂ concentration. This is the conclusion reached by a European research team led by the OCCR.
A new measurement technology developed at the University of Bern provides unique insights into the climate of the past. Previous CO₂ concentrations in the atmosphere could be reconstructed more accurately than ever before, thanks to high-resolution measurements made on an Antarctic ice core. The study, which analyzed the Earth’s atmospheric composition between 330,000 and 450,000 years ago, was made possible by the commitment of experts, and their decades of experience, at the University of Bern. The results of the study have been published in Science.
Melting ice masses disturbed the ocean circulation
In 2008, the Bern ice core specialists were able to show that the CO₂ concentration in the atmosphere during the last 800,000 years was consistently much lower than today. Since then, the ice core experts have built upon those findings enabling a much more detailed reconstruction of the 330,000 to 450,000 year time window. Until now, the maximum speed and frequency of naturally occurring centennial scale jumps in the CO₂ concentration remained unknown. This study shows that abrupt CO₂ rises are a pervasive feature of our climate system and that they can even occur during interglacial periods. "Until now, it had been assumed that the climate was very stable during previous interglacial periods and that there were no abrupt changes in the atmospheric CO₂ concentration," explains Christoph Nehrbass-Ahles, lead author of the study, who earned a doctorate from the University of Bern and is now based at the University of Cambridge. According to Nehrbass-Ahles, the abrupt rises were always evident when melting ice masses in Greenland or Antarctica considerably disturbed the ocean circulation. If the CO₂ in the atmosphere rose quickly, simultaneous changes in the Atlantic Ocean's circulation could also be detected.
CO₂ increase was ten times slower than today
The fact that rapid CO₂ jumps could be detected not only during glacial periods but also during two previous interglacial periods surprised the researchers. "We measured these events in the ice several times and always came to the same conclusion," explains Nehrbass-Ahles. Why the CO₂ concentration in the atmosphere suddenly rose during previous interglacial periods cannot be conclusively explained by the researchers. "We do not know why this happened yet," explains Thomas Stocker, OCCR member and co-author of the study: "This raises new research questions." However, the CO₂ jumps in previous interglacial periods are far exceeded by the current development: "These natural jumps in the CO₂ concentration in the atmosphere happened almost ten times slower than the human-driven increase over the last decade," Nehrbass-Ahles emphasizes.
The largest jump in the past corresponds to the current CO₂ emissions over only six years
The researchers compared the CO₂ jumps of the past with the ongoing human-driven rise of CO₂ concentration in the atmosphere. According to Stocker, the largest centennial CO₂ jump in the past was around 15 ppm (parts per million is the unit for atmospheric CO₂ concentration), which is approximately equivalent to the increase caused by humankind over the last of six years. "This may not seem significant at first glance," says Stocker, "but in light of the quantities of CO₂ that we are still allowed to emit in order to achieve the 1.5°C climate target agreed in Paris, such increases are definitely relevant." The findings of this study put us under even greater pressure to protect the climate.
The study was made possible by long-term contributions from the Swiss National Science Foundation and the European Commission within the framework of the European Project for Ice Coring in Antarctica (EPICA).
(Source: Universtiy of Bern)