Savannah River

Total streamflow across the Savannah River was last observed at 168,940 cfs, and is expected to yield approximately 335,088 acre-ft of water today; about 97% of normal. Average streamflow for this time of year is 174,660 cfs, with recent peaks last observed on 2016-01-12 when daily discharge volume was observed at 642,100 cfs.

Maximum discharge along the river is currently at the Savannah River At Fort Pulaski reporting a streamflow rate of 155,000 cfs. However, the streamgauge with the highest stage along the river is the Savannah River At Augusta with a gauge stage of 96.71 ft. This river is monitored from 6 different streamgauging stations along the Savannah River, the highest being situated at an altitude of 121 ft, the Savannah River At Augusta.

It originates in the mountains of North Carolina and flows for over 300 miles before eventually joining the Atlantic Ocean. The river has played an important role throughout history, serving as a transportation route for Native Americans, European colonizers, and American settlers. Today, the river is used for a variety of purposes, including hydroelectric power generation, irrigation, and recreation. The Savannah River is home to several major reservoirs, including Lake Hartwell, Lake Thurmond, and Lake Russell, which were created by dams constructed for flood control and hydroelectric power. These reservoirs provide a source of drinking water and support recreational activities such as boating, fishing, and swimming. Agriculturally, the river supports the production of crops such as cotton, peanuts, and soybeans in the surrounding areas.