Total streamflow across the Tippecanoe River was last observed at 1,185 cfs, and is expected to yield approximately 2,349 acre-ft of water today; about 34% of normal. River levels are low and may signify a drought. Average streamflow for this time of year is 3,489 cfs, with recent peaks last observed on 2018-02-22 when daily discharge volume was observed at 33,670 cfs.

Maximum discharge along the river is currently at the Tippecanoe River At Buffalo reporting a streamflow rate of 563 cfs. This is also the highest stage along the Tippecanoe River, with a gauge stage of 7.5 ft at this location. This river is monitored from 6 different streamgauging stations along the Tippecanoe River, the highest being situated at an altitude of 852 ft, the Tippecanoe River At North Webster.

The Tippecanoe River is a 225-mile-long river that flows through northern Indiana, originating from the wetlands in Tippecanoe Lake. The river has a rich history, playing a significant role in transportation, trade, and the fur trapping industry during the early 19th century. It is also known for its connection to the famous Battle of Tippecanoe, fought between the Shawnee and US forces in 1811. The river flows through several reservoirs, including the Norway, Oakdale, Winona, and Dewart Lake reservoirs, which are used for flood control, water supply, and recreational activities such as boating, fishing, and camping. The Tippecanoe River is also critical for agriculture, supplying water for crop irrigation in the surrounding areas. The river is home to a diverse range of flora and fauna, providing habitat for various species of fish, birds, and mammals.