Total streamflow across the Raquette River was last observed at 8,230 cfs, and is expected to yield approximately 16,324 acre-ft of water today; about 264% of normal. River levels are high. Average streamflow for this time of year is 3,112 cfs, with recent peaks last observed on 2011-05-01 when daily discharge volume was observed at 34,700 cfs.

Maximum discharge along the river is currently at the Raquette River At Raymondville Ny reporting a streamflow rate of 3,210 cfs. However, the streamgauge with the highest stage along the river is the Raquette River At Piercefield Ny with a gauge stage of 6.88 ft. This river is monitored from 3 different streamgauging stations along the Raquette River, the highest being situated at an altitude of 1,502 ft, the Raquette River At Piercefield Ny.

The Raquette River is a 146-mile-long river in northern New York that flows from the Adirondack Mountains to the Saint Lawrence River. Historically, the river was used for transportation by Native American tribes and European settlers. The river's hydrology is heavily influenced by rainfall and snowmelt, making it prone to seasonal flooding. Numerous reservoirs and dams have been constructed along the river for hydroelectric power generation, including the Colton, Higley, and Piercefield Dams. These reservoirs also provide recreational opportunities such as fishing, boating, and swimming. Additionally, the river supports local agriculture and is used for irrigation and water supply.