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Climate



Warming trends in the western U.S. have already produced significant changes in snow-driven hydrology. In the past 50 years, dates of peak snow accumulation and of peak snow melt derived stream flow have shifted earlier, typically by 10-40 days, and spring snow pack has decreased in most of the West (total decrease of 11% since 1950). Although a direct causal connection between the observed changes and rising concentrations of greenhouse gases cannot yet be established, it is likely that the declines reflect human influence. In many important respects, these observed changes are consistent with projections of future changes in a warming world, where losses in the West’s total April 1 snow pack are likely to exceed 40% by the 2050s. These observed changes point toward further reductions in summer water supply and increased demand.

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     Page last modified on Monday April 19, 2004.