Chenango River River Levels

Last Updated: January 27, 2026

The Chenango River is a 90-mile-long river that flows through central New York, draining into the Susquehanna River.



15-Day Weather Outlook


Summary

Total streamflow across the Chenango River was last observed at 3,667 cfs, and is expected to yield approximately 7,273 acre-ft of water today; about 85% of normal. Average streamflow for this time of year is 4,322 cfs, with recent peaks last observed on 2011-09-08 when daily discharge volume was observed at 64,910 cfs.

Maximum discharge along the river is currently at the Chenango River Near Chenango Forks Ny reporting a streamflow rate of 2,710 cfs. However, the streamgauge with the highest stage along the river is the Chenango River At Sherburne Ny with a gauge stage of 4.35 ft. This river is monitored from 3 different streamgauging stations along the Chenango River, the highest being situated at an altitude of 1,039 ft, the Chenango River At Sherburne Ny.

River Details

Last Updated 2026-01-21
Discharge Volume 7,273 ACRE-FT
Streamflow 3,667.0 cfs
-1114.0 cfs (-23.3%)
Percent of Normal 84.84%
Maximum 64,910.0 cfs
2011-09-08
Seasonal Avg 4,322 cfs
       
River Streamflow Levels
Streamgauge Streamflow Gauge Stage 24hr Change (%) % Normal Minimum (cfs) Maximum (cfs) Air Temp Elevation
Chenango River At Sherburne Ny
USGS 01505000
501 cfs 4.35 ft -17.46
Chenango River At Greene Ny
USGS 01507000
957 cfs 4.33 ft -17.5
Chenango River Near Chenango Forks Ny
USGS 01512500
2710 cfs 4.13 ft -13.14
Seasonal Discharge Comparison
Maximum Streamflow Discharge
Streamflow Elevation Profile

The Chenango River is a 90-mile-long (140 km) tributary of the Susquehanna River in central New York in the United States. It drains a dissected plateau area in upstate New York at the northern end of the Susquehanna watershed.
Named after the Oneida word for bull thistle, in the 19th century the Chenango furnished a critical link in the canal system of the northeastern United States. The Chenango Canal, built from 1836–1837 between Utica and Binghamton, connected the Erie Canal in the north to the Susquehanna River. The canal was rendered obsolete by railroads and was abandoned in 1878.
Flooding is often a concern during the spring and fall.