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Solomon's paper concludes that if CO2 is allowed to peak at 450-600 parts per million, the results would include persistent decreases in dry-season rainfall that are comparable to the 1930s North American Dust Bowl in zones including southern Europe, northern Africa, southwestern North America, southern Africa and western Australia. Gerald Meehl, a senior scientist at the National Center for Atmospheric Research, said, "The real concern is that the longer we wait to do something, the higher the level of irreversible climate change to which we'll have to adapt." Meehl was not part of Solomon's research team. While scientists have been aware of the long-term aspects of climate change, the new report highlights and provides more specifics on them, said Kevin Trenberth, head of climate analysis at the center. "This aspect is one that is poorly appreciated by policymakers and the general public and it is real," said Trenberth, who was not part of the research group. "The temperature changes and the sea level changes are, if anything underestimated and quite conservative, especially for sea level," he said. While he agreed that the rainfall changes mentioned in the paper are under way, Trenberth disagreed with some details of that part of the report. "Even so, there would be changes in snow (to rain), snow pack and water resources, and irreversible consequences even if not quite the way the authors describe," he said. "The policy relevance is clear: We need to act sooner ... because by the time the public and policymakers really realize the changes are here it is far too late to do anything about it. In fact, as the authors point out, it is already too late for some effects." Co-authors of the paper were Gian-Kaspar Plattner and Reto Knutti of the Swiss Federal Institute of Technology in Zurich and Pierre Friedlingstein of the National Institute for Scientific Research, Gif sur Yvette, France. The research was supported by the Office of Science at the Department of Energy. ___ On the Net: PNAS: http://www.pnas.org/
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