Predicted net efflux of radiocarbon from the ocean and increase in atmospheric radiocarbon content
Key finding. A global carbon-cycle model predicts that atmospheric radiocarbon content will reach a minimum and begin to increase within the next few years under a business-as-usual emissions scenario — even though fossil fuels contain no radiocarbon at all — because rising atmospheric CO2 drives a net flux of carbon-14 out of the ocean and land biosphere.
What question did this research address?
Before human interference, radiocarbon production in the stratosphere nearly balanced its flux into the ocean and land biosphere, which in turn nearly balanced radioactive decay. Land-use change, fossil-fuel burning, and atmospheric nuclear tests broke that balance.
Bomb testing raised atmospheric carbon-14 by about 80% by the mid-1960s, and it has been falling since as the excess enters the oceans and biosphere. This paper asked what happens next, and why the historical record does not look the way naive reasoning predicts.
What did we find?
The puzzle the paper starts from is quantitative. Atmospheric radiocarbon fell far less between pre-industrial times and 1950 than the roughly 10% rise in atmospheric CO2 over the same period would lead one to expect from dilution alone.
Most of that discrepancy is explained by radiocarbon fluxes out of the land biosphere and oceans induced by the rising burden of ordinary carbon dioxide — an effect recognized since the 1950s and here quantified in a full carbon-cycle model.
The same mechanism dominates the future. Continued fossil-fuel burning indirectly causes a significant increase in atmospheric carbon-14 content, despite fossil carbon being devoid of it.
Under business-as-usual, the crossover comes soon: the bomb-radiocarbon decline reaches its minimum and reverses within a few years of the paper.
The model puts the turning point at 1998 — the year atmospheric carbon-14 content starts rising again, reversing a decline that began in the mid-1960s, and a prediction the authors note will soon be testable.
Beyond that, the ocean itself changes sign. The fossil-fuel-induced radiocarbon flux out of the ocean is predicted to exceed the natural flux into it by about 2030 and the natural plus bomb flux by about 2050, making the ocean a net source of carbon-14 to the atmosphere by the middle of the century.
Of the increase in atmospheric radiocarbon between 1945 and 1995, about 30% is attributed to land-use change and fossil-fuel burning, with the remaining 70% from atmospheric nuclear detonations.
Why does it matter?
Radiocarbon is the main tracer used to calibrate how fast ocean models ventilate the deep sea, so getting its budget right propagates into every estimate of ocean carbon uptake built on it.
The result is counter-intuitive in a way that is instructive. Adding carbon with no radiocarbon in it raises the atmosphere's radiocarbon content, because the isotopic effect of disturbing the reservoirs outweighs the dilution.
It also bears on radiocarbon dating of recent material, where the atmospheric curve reversing direction means a measured value no longer maps to a single date.
Citation
Ken Caldeira, Greg H. Rau, and Philip B. Duffy (1998). Predicted net efflux of radiocarbon from the ocean and increase in atmospheric radiocarbon content. Geophysical Research Letters 25, 3811-3814.
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- Sensitivity of simulated CFC-11 distributions in a global ocean model to the treatment of salt rejected during sea-ice formation (Caldeira and Duffy, 1998)
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- The role of the Southern Ocean in uptake and storage of anthropogenic carbon dioxide (Caldeira and Duffy, 2000)