May 30, 2013
"This study ultimately shows why waiting for certainty will fail as a strategy," lead author Roger Bodman from Victoria University said. "Some uncertainty will always remain, meaning that we need to manage the risks of warming with the knowledge we have."
According to the research the wide temperature range (2-6 degrees Celsius) is due to three factors: climate sensitivity to greenhouse gas emissions, the unpredictability of the carbon cycle, and aerosols, which cool the planet. These three factors "remain highly uncertain," the researchers write, "but historical observations of temperature and carbon dioxide imply a trade–off between them so that temperature projections are more certain than they would be considering each factor in isolation."
Using historical data on carbon dioxide concentrations and temperature changes, the researchers employed a simplified climate model to predict how much more the Earth is likely to warm over the next 87 years. Already the Earth has warmed around 0.8 degrees Celsius (1.44 degrees Fahrenheit) over the last hundred years. This warming has led to shrinking glaciers, vanishing Arctic sea ice, increased risk of floods and drought, more extreme storms, and rising sea levels.
According to the study it's unlikely that temperatures will rise more than six degrees Celsius (11 degrees Fahrenheit) this century. But the World Bank has recently noted that a rise in 4 degrees Celsius would lead to a world wholly different than the one we inhabit today, including agricultural collapse, economic turmoil, and mass extinction on land and sea.
"Our results reconfirm the need for urgent and substantial reductions in greenhouse gas emissions if the world is to avoid exceeding the global warming target of 2 degrees needed to minimize dangerous climate change," co-author David Karoly from the University of Melbourne said.
CITATION: Roger W. Bodman, Peter J. Rayner, and David J. Karoly. Uncertainty in temperature projections reduced using carbon cycle and climate observations. Nature Climate Change (2013). doi:10.1038/nclimate1903
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