The unique topographic features of the northern Great Plains' prairie pothole regions, the soil moisture setting, the snowpack and snowmelt conditions, rainfall events, and the release from reservoirs located north of Stratford on the James River all combined to determine how long the flood would last. As several sites north of Stratford, South Dakota have experienced a substantial rise in flooding and reservoir inflow since the early 1990s, this flooding event is not an isolated event. In addition to examining the circumstances and potential causes of these occurrences, this presentation will consider how climate change may be affecting the northern Great Plains prairie pothole regions including the flooding response to large precipitation events.

