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How anthropogenic climate change will affect hydroclimate inthe arid regions of southwestern North America has implicationsfor the allocation of water resources and the course of regionaldevelopment. Here we show that there is a broad consensus amongclimate models that this region will dry in the 21st centuryand that the transition to a more arid climate should alreadybe under way. If these models are correct, the levels of aridityof the recent multiyear drought or the Dust Bowl and the 1950sdroughts will become the new climatology of the American Southwestwithin a time frame of years to decades.
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