Streamflow levels across
Oregon
are currently
111.0% of normal, with the
Columbia River @ Beaver Army Terminal Nr Quincy
reporting the highest discharge in the state with
291000cfs and gauge stage of 1.23 ft.
Meanwhile, the
Bull Run River Near Bull Run
is seeing a spike in streamflows today after experiencing a
222.83%
increase since yesterday, and currently running at
410cfs.
Maximum gauge stage in the state was last observed at the
Sevenmile Cnl At Dike Rd Br, currently reporting a stage of
4139.16ft.
The
North Umpqua River At Toketee Falls Oreg.
in the
North Umpqua
watershed
is surging for this time of year at
585cfs, about
316.31% of normal.
Oregon's surface flows are impacted by its varied hydrology and climate characteristics. Major rivers and tributaries include the Columbia, Snake, and Willamette. Reservoirs and dams, such as the Bonneville Dam and the Dalles Dam, have been constructed along these waterways to provide hydroelectric power and irrigation. Snowpack is a crucial factor in Oregon's water supply, with the majority of the state's precipitation occurring in the winter months. In recent years, lower than average snowpack levels have led to drought conditions and water shortages. The Klamath Basin has been a focal point in the state's water management, with disputes arising between farmers, tribes, and environmental advocates over water allocation. Overall, Oregon's water resources are complex and often contentious, requiring careful management and planning.