New Forecast: Hot and Hotter
Dangerous emissions.
Experiments at this meadow in the Colorado Rockies show that, under the temperatures corresponding to climate models estimates for about 2050, soils release carbon dioxide.
Credit: JOHN HARTE
Currently, the Intergovernmental Panel on Climate Change estimates that the global average temperature could increase as much as 5.8 degrees Celsius by the end of the 21st century. But these estimates don't factor in some feedback mechanisms that may be triggered by rising temperatures. For instance, accelerated decomposition in soils and changes in ocean chemistry may add considerably to greenhouse gases and further intensify warming. Two studies published 26 May in Geophysical Research Letters attempt to translate these potential impacts into hard numbers.
In the first study, biogeochemists Margaret Torn of Lawrence Berkeley National Laboratory in California and John Harte of the University of California, Berkeley, used Antarctic ice cores to estimate the amount of greenhouse gases released into the atmosphere over the past 420,000 years, allowing them to predict the impact of future climate-CO2 feedbacks. Combining these estimates with standard assumptions from climate models, they calculated the amplification in global temperatures attributable to greenhouse gas feedback. They found that a doubling of current CO2 levels would boost temperatures by 1.6 to 6 degrees Celsius, and by 2100 the gain could be as much as 7.7 degrees C.
Torn notes that many feedback mechanisms remain poorly understood, and uncertainties abound in trying to predict their effects on climate. But she believes the findings indicate "that we will experience more severe, not less severe, climate change than is currently forecast."
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