At the end of the dry season: CO₂ pulses over Australia

This text is based on a press release kindly made available to us by the University of Heidelberg.

End-of-dry-season CO₂ pulses recur each year in the atmosphere above the Australian continent, a discovery made by an international research team including scientists from MPI-BGC. To investigate the carbon fluxes over Australia, the researchers studied atmospheric CO₂ measurements. Their analyses show that CO₂ emissions spike when heavy rain falls on dried-out soil, thus activating microorganisms in that soil. The findings suggest that dry regions have a greater influence on the variations in the global carbon cycle than previously thought.

The Australian continent is dominated by dry ecosystems and widely varying precipitation patterns. Generally, at the end of the dry season – when the first rains begin to fall – CO₂ emissions over Australia rise sharply. “This effect is well-known at the local level, but it was never observed at the continental level,” states Eva-Marie Metz, a doctoral candidate at the Institute of Environmental Physics at Heidelberg University. Data on the atmospheric CO₂ concentrations obtained from the Greenhouse Gases Observing Satellite (GOSAT) were analysed. Using the satellite data from 2009 to 2018, the scientists found that the seasonal pattern of CO2 concentrations over Australia was much more dynamic than previously assumed.

Until now, the lack of measurement data on ground hampered uncovering the mechanisms that cause these variations. The research team fed the GOSAT satellite data into an atmospheric inversion model, which is used to estimate the CO₂ flux at the ground level. It became clear that there must be an undiscovered mechanism of CO2 release in Australian terrestrial ecosystems. Further studies showed that the concentrations of CO₂ always rise when dry soils are rewetted by heavy rainfall. This causes the so-called “Birch Effect”. Soil microbes that are inactive when dry are reactivated by the

moisture and multiply, causing the soil to “breathe” and release CO₂ . Plant photosynthesis does not begin until later, so carbon dioxide is not bound at the end of the dry season, thus causing the seasonally rapid rise in CO₂ that the international team of researchers was able to discern on the continental level.

Their investigations have provided an explanation on how the variations in the carbon fluxes from land to atmosphere occur. These results are significant because they suggest that dry regions – such as are dominant in Australia – have a greater influence on the variations of the global carbon cycle than previously believed. “Our findings, the first on a continental scale, can be used for climate modelling and thus contribute to a better understanding of the global climate-carbon feedbacks,” explains Prof Butz from Heidelberg University.

The research results were published in the journal “Science”.  Several researchers from different departments and groups of the Max Planck Institute for Biogeochemistry in Jena participated in the research. Funding was provided by the German Research Foundation, among others.