Total streamflow across the Whitewater River was last observed at 1,137 cfs, and is expected to yield approximately 2,254 acre-ft of water today; about 86% of normal. Average streamflow for this time of year is 1,314 cfs, with recent peaks last observed on 2019-02-08 when daily discharge volume was observed at 51,883 cfs.

Maximum discharge along the river is currently at the Whitewater R A Windy Point Main Channel Ca reporting a streamflow rate of 588 cfs. However, the streamgauge with the highest stage along the river is the Whitewater R A Windy Point Overflow Channel Ca with a gauge stage of 12.1 ft. This river is monitored from 9 different streamgauging stations along the Whitewater River, the highest being situated at an altitude of 1,242 ft, the Whitewater R At Towanda.

The Whitewater River is a 30-mile-long tributary of the Little Miami River in southwestern Ohio. It is a popular destination for whitewater kayaking and canoeing due to its fast-moving rapids and scenic beauty. The river's name is believed to have originated from the white foam created by the rapids. The river's hydrology is primarily influenced by rainfall and snowmelt. The river flows through several reservoirs, including East Fork Lake and William H. Harsha Lake, which are used for flood control, water supply, and recreational purposes. The river's water is also used for agricultural purposes such as irrigation. The river has a rich history, having played a crucial role in the development of the region's early industries, including mills and factories. Today, the Whitewater River is a popular recreational destination enjoyed by many outdoor enthusiasts.