Total streamflow across the Yockanookany River was last observed at 527 cfs, and is expected to yield approximately 1,046 acre-ft of water today; about 22% of normal. River levels are low and may signify a drought. Average streamflow for this time of year is 2,375 cfs, with recent peaks last observed on 2020-02-13 when daily discharge volume was observed at 29,200 cfs.

Maximum discharge along the river is currently at the Yockanookany River Nr Ofahoma reporting a streamflow rate of 458 cfs. This is also the highest stage along the Yockanookany River, with a gauge stage of 9.41 ft at this location. This river is monitored from 2 different streamgauging stations along the Yockanookany River, the highest being situated at an altitude of 385 ft, the Yockanookany River Nr Kosciusko.

The Yockanookany River, located in central Mississippi, stretches for 63 miles before emptying into the Pearl River. Historically, the river was used for transportation by Native Americans and early European settlers. Today, it is primarily used for recreation and agriculture. The river flows through several reservoirs, including the 9,000-acre Ross R. Barnett Reservoir, which was constructed in the 1960s to provide flood control, water supply, and recreational opportunities. The Mary Ricks Thornton Lake is another smaller reservoir used for recreation, located near the town of Canton. The Yockanookany is also an important water source for agricultural irrigation in the region. The river is popular for fishing, kayaking, and other outdoor activities, with several public access points and campgrounds available for visitors.