Soil will absorb less atmospheric carbon than expected this century – ‘The problems of carbon emission and climate change are worse than what we expected’Posted by Jim at Sunday, September 25, 2016
IRVINE, California, 22 September 2016 – By adding highly accurate radiocarbon dating of soil to standard Earth system models, environmental scientists from the University of California, Irvine and other institutions have learned a dirty little secret: The ground will absorb far less atmospheric carbon dioxide this century than previously thought.
Researchers used carbon-14 data from 157 sample sites around the world to determine that current soil carbon is about 3,100 years old – rather than the 450 years stipulated by many Earth system models.
“This work indicates that soils have a weaker capacity to soak up carbon than we have been assuming over the past few decades,” said UCI Chancellor’s Professor of Earth system science James Randerson, senior author of a new study on the subject to be published Friday in the journal Science. “It means we have to be even more proactive in finding ways to cut emissions of fossil fuels to limit the magnitude and impacts of climate warming.”
Through photosynthesis, plants absorb CO2 from the air. When trees and vegetation die and decay, they become part of the soil, effectively locking carbon on or beneath the Earth’s surface – keeping it out of the atmosphere, where it contributes to global warming. In their study, the researchers showed that since this process unfolds over millennia versus decades or centuries, we should expect less of this land carbon sequestration in the 21st century than suggested by current Earth system models.
“A substantial amount of the greenhouse gas that we thought was being taken up and stored in the soil is actually going to stay in the atmosphere,” said study co-author Steven Allison, UCI associate professor of ecology & evolutionary biology and Earth system science.
In recent years, scientists have used highly complex, computer-based Earth system models – compilations of code integrating data on the planet’s oceans, land surfaces, ice masses, atmosphere and biological systems – to draw conclusions about potential future changes in regional and global temperatures, drought, sea levels, and other phenomena.
The models don’t explicitly provide the age of carbon in soils, but lead author Yujie He, a UCI postdoctoral scholar when the study was conducted, said that she and her colleagues figured out a way to improve them through simplification and the addition of dating methods well-established in the scientific community.
“Radiocarbon is an excellent tool for understanding soil dynamics,” He said. “Our study demonstrated that by working to reduce the complexity of Earth system models and combining observational data, we could get them to reveal surprising findings.”
The authors said that adding more carbon to that which has been in the ground for thousands of years is problematic given the pace at which the Earth seems capable of integrating it.
“If we waited 300, 400, 1,000 years, then that carbon – we think – would go into the soil. But that’s not going to help us in dealing with climate change, which is happening now,” Allison said. “You have to do a lot of risk assessment to say, well, what’s the actual cost of just waiting for that sequestration, and what policies should we implement to avoid that possible cost? That’s outside the realm of our actual work here, but what we can say is that the problems of carbon emission and climate change are worse than what we expected previously.”
Also contributing to the study were Susan Trumbore of the Max Planck Institute for Biogeochemistry, Margaret Torn and Lydia Vaughn of the Lawrence Berkeley National Laboratory, and Jennifer Harden of Stanford University and the U.S. Geological Survey.
ABSTRACT: Soil is the largest terrestrial carbon reservoir and may influence the sign and magnitude of carbon cycle–climate feedbacks. Many Earth system models (ESMs) estimate a significant soil carbon sink by 2100, yet the underlying carbon dynamics determining this response have not been systematically tested against observations. We used 14C data from 157 globally distributed soil profiles sampled to 1-meter depth to show that ESMs underestimated the mean age of soil carbon by a factor of more than six (430 ± 50 years versus 3100 ± 1800 years). Consequently, ESMs overestimated the carbon sequestration potential of soils by a factor of nearly two (40 ± 27%). These inconsistencies suggest that ESMs must better represent carbon stabilization processes and the turnover time of slow and passive reservoirs when simulating future atmospheric carbon dioxide dynamics.