| Water Planners Call For Fundamental Shift To 
    Deal With Changing Climate 2/1/2008
 
 Seattle, WA — The past is no longer a reliable base on which to plan the 
    future of water management. So says a new perspectives piece written by a 
    prominent group of hydrologists and climatologists, recently published in 
    Science, that calls for fundamental changes to the science behind water 
    planning and policy.
 
 "With the climate changing, past years aren't necessarily representative of 
    the future anymore," said co-author Dennis Lettenmaier, a professor of civil 
    engineering at the University of Washington. "This paper says that the way 
    business has been done in the past will no longer work in a changing 
    climate."
 
 Global spending on water infrastructure is currently more than $500 billion 
    per year. Until now, managers at municipal water boards, the Army Corps of 
    Engineers, the U.S. Bureau of Reclamation and other federal, state and local 
    agencies have operated on the premise that historical patterns could be 
    counted on to continue. The assumption was that variability from year to 
    year occurred within stationary, unchanging patterns.
 
 But human-induced changes to Earth's climate have begun to shift the 
    averages and the extremes for rainfall, snowfall, evaporation and stream 
    flows, the authors write. These are crucial factors when planning for floods 
    or droughts, choosing the size of water reservoirs or deciding how much 
    water to allocate for residential, industrial and agricultural uses.
 
 "Historically, looking back at past observations has been a good way to 
    estimate future conditions," said lead author Christopher Milly, a research 
    hydrologist with the U.S. Geological Survey. "But climate change magnifies 
    the possibility that the future will bring droughts or floods you never saw 
    in your old measurements."
 
 The old way of doing business is dead, the authors write. And it cannot be 
    revived. Even with an aggressive reduction in greenhouse gas emissions, 
    warming will persist and global water patterns will continue to show 
    never-before-seen behavior.
 
 The authors thus propose a planning framework like the Harvard Water 
    Program, a project from the late 1950s to the early 1960s in which 
    scientists and engineers hammered out the basis for the current 
    water-management policies. The authors call for a renewed effort in the 
    spirit of the earlier program that would incorporate shifting averages and 
    variability.
 
 Not all regions will experience the same changes in flows.
 
 "Our best current estimates are that water availability will increase 
    substantially in northern Eurasia, Alaska, Canada and some tropical regions, 
    and decrease substantially in southern Europe, the Middle East, southern 
    Africa and southwestern North America," Milly said. Drying regions will 
    likely also experience more frequent droughts, he said.
 
 In the West, changes in precipitation and the timing of snowmelt now seem 
    likely to affect seasonal flow patterns that are critical to salmon runs, 
    water supply and other water uses, Lettenmaier said.
 
 "For agencies like the Army Corps of Engineers and the Bureau of 
    Reclamation, this would mean fundamental changes in the way they do 
    business," he said. "If you look at plans by those agencies for management 
    of the Columbia River, essentially they've ignored climate change. For 
    instance, until quite recently, the National Marine Fisheries Service didn't 
    even mention what climate change might mean for rehabilitation of fish 
    runs."
 
 Asked whether the new paper would prompt changes in management practices, 
    Lettenmaier said: "I think so. I think it will become increasingly hard to 
    ignore climate change in water management."
 
 Co-authors are Julio Betancourt and Robert Hirsch at the U.S. Geological 
    Survey, Malin Falkenmark at the Stockholm International Water Institute in 
    Sweden, Zbigniew Kundzewicz at the Potsdam Institute for Climate Impact 
    Research in Germany and Ronald Stouffer at the Geophysical Fluid Dynamics 
    Laboratory in Princeton, N.J.
 
 SOURCE: University of Washington
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