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- W2032439487 abstract "Climate change is expected to alter the time and space characteristics of the global hydrologic cycle and to impact regional water supplies. The Upper Deschutes Basin is in one of Oregon’s fastest growing regions, and the increasing population is straining regional water resources. Surface water is fully allocated and increased groundwater use will require careful management to offset seasonal or long-term declines in aquifers or the depletion of stream flow. While altered temperature and precipitation accompanying global change are both concerns, the watershed is more sensitive to changes in precipitation than in temperature. Watershed climate simulation reveals a 25 percent increase in mean monthly runoff, and extremely high monthly runoff is four times more frequent. These changes indicate an increased risk of winter floods, greater spring and summer runoff, and a shift in the occurrence of the minimum runoff month to earlier in the year. Increased potential evapotranspiration, a decrease in the amount of precipitation stored as snow, and changes in the amount and timing of runoff will constrain water development options for humans, agriculture, and regional fisheries. Water restrictions will magnify water-use conflicts in the watershed and increase the risk of regional economic discord." @default.
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- W2032439487 date "2001-01-01" @default.
- W2032439487 modified "2023-10-17" @default.
- W2032439487 title "Water Supply and Climate Change in the Upper Deschutes Basin, Oregon" @default.
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- W2032439487 doi "https://doi.org/10.1353/pcg.2001.0011" @default.
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