Total streamflow across the Gasconade River was last observed at 6,356 cfs, and is expected to yield approximately 12,607 acre-ft of water today; about 70% of normal. River levels are low and may signify a drought. Average streamflow for this time of year is 9,131 cfs, with recent peaks last observed on 2015-12-30 when daily discharge volume was observed at 282,000 cfs.

Maximum discharge along the river is currently at the Gasconade River Near Rich Fountain reporting a streamflow rate of 2,940 cfs. This is also the highest stage along the Gasconade River, with a gauge stage of 4.55 ft at this location. This river is monitored from 3 different streamgauging stations along the Gasconade River, the highest being situated at an altitude of 845 ft, the Gasconade River Near Hazelgreen.

The Gasconade River is a 280-mile-long river in central Missouri, USA. It was named after the Gasconade people who originally lived in the area. The river is a popular destination for fishing, canoeing, and camping. The hydrology of the Gasconade River is characterized by seasonal variations in flow, with high levels during spring and summer due to snowmelt and precipitation. The river has four main reservoirs/dams: Bagnell Dam, Harry S. Truman Dam, Pomme de Terre Dam, and Lake of the Ozarks Dam. These dams provide flood control, power generation, and recreational opportunities. The Gasconade River watershed is also an important agricultural area, with corn, soybeans, and livestock being the primary agricultural products.