Streamflow levels across
South Dakota
are currently
73.0% of normal, with the
James R Near Scotland Sd
reporting the highest discharge in the state with
627cfs and gauge stage of 4.62 ft.
Meanwhile, the
James R Near Stratford Sd
is seeing a spike in streamflows today after experiencing a
2.41%
increase since yesterday, and currently running at
298cfs.
Maximum gauge stage in the state was last observed at the
James River At Nd-Sd State Line, currently reporting a stage of
88ft.
The
James R Near Forestburg Sd
in the
Lower James
watershed
is surging for this time of year at
518cfs, about
57.79% of normal.
South Dakota has a humid continental climate with four distinct seasons. The Missouri River, which forms the eastern border of the state, is the largest and most significant surface flow. It is subject to extreme flooding during spring and summer due to snowmelt and heavy rainfall. Other major rivers include the Cheyenne, James, and Big Sioux. The state has several reservoirs and dams, including the Oahe, Fort Randall, and Big Bend dams, which provide flood control, irrigation, and hydroelectric power. South Dakota's hydrology is influenced by its topography, soil type, and vegetation cover, which affect the amount and rate of water infiltration and runoff. The state's snowpack and precipitation patterns are important factors in determining water availability and storage.