Streamflow levels across
Oklahoma
are currently
63.0% of normal, with the
Arkansas River Near Muskogee
reporting the highest discharge in the state with
7330cfs and gauge stage of 18.39 ft.
Meanwhile, the
Canadian River Near Whitefield
is seeing a spike in streamflows today after experiencing a
335.81%
increase since yesterday, and currently running at
1290cfs.
Maximum gauge stage in the state was last observed at the
Canadian River At Norman, currently reporting a stage of
86.54ft.
The
Arkansas River Near Haskell
in the
Polecat-Snake
watershed
is surging for this time of year at
4010cfs, about
100.6% of normal.
Oklahoma has a humid subtropical climate with frequent thunderstorms and occasional tornadoes. The state is home to major surface flows, including the Arkansas, Canadian, and Red Rivers. These rivers are subject to flooding during periods of heavy rainfall. Major reservoirs and dams, such as the Keystone Dam on the Arkansas River, help to manage flood control and provide water for agriculture and drinking water. Oklahoma's hydrology is influenced by its geology, which includes karst formations and oil and gas extraction. Watershed and snowpack data are not significant factors in Oklahoma's hydrology due to its low snowfall and lack of major mountain ranges.