In general, the models show that existing climate zones will shift toward higher latitudes and higher elevations, squeezing out the climates at the extremes--tropical mountaintops and the poles--and leaving room for unfamiliar climes and new ecological niches around the equator.
The work, by researchers at the University of Wisconsin-Madison and the University of Wyoming, appears online in the journal Proceedings of the National Academy of Sciences (PNAS) during the week of March 26. The National Science Foundation (NSF) funded the research.The most severely affected parts of the world span both heavily populated regions, including the southeastern United States, southeastern Asia, and parts of Africa, and known hotspots of biodiversity, such as the Amazonian rainforest and African and South American mountain ranges.
The patterns of change foreshadow significant impacts on ecosystems and conservation. "There is a close correspondence between disappearing climates and areas of biodiversity," says University of Wisconsin at Madison geographer Jack Williams, primary author of the paper, which could increase risk of extinction in the affected areas.
For example, the Andes, Central America, South Africa and the Indonesian Archipelago are all hotspots of biological diversity. The projected disappearance of the climates unique to these regions places some species at risk of extinction."
As this research shows, studies integrating paleoclimate data, mathematical modeling and ecological principles provide insights into climate cause-and-effect that are of great practical consequence," says David Verardo, program director for paleoclimate at NSF,Williams and his colleagues foresee the appearance of novel climate zones on up to 39 percent of the world's land surface area by 2100, if current rates of carbon dioxide and other greenhouse gas emissions continue, and the global disappearance of up to 48 percent of current land climates.
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