SNOFLO



CHENANGO RIVER

RIVER LEVELS
April 29, 2025


Total streamflow across the Chenango River was last observed at 3,528 cfs, and is expected to yield approximately 6,998 acre-ft of water today; about 76% of normal. Average streamflow for this time of year is 4,617 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 2,340 cfs. This is also the highest stage along the Chenango River, with a gauge stage of 4.23 ft at this location. 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.

Last Updated 2025-04-29
Discharge Volume 6,998 ACRE-FT
Streamflow 3,528.0 cfs
-631.0 cfs (-15.17%)
Percent of Normal 76.42%
Maximum 64,910.0 cfs
2011-09-08
Seasonal Avg 4,617 cfs
       
River Streamflow Levels
Created with Highcharts 8.0.0Total River Discharge (cfs)20. Apr21. Apr22. Apr23. Apr24. Apr25. Apr26. Apr27. Apr28. Apr29. Apr02.5k5k
Seasonal Discharge Comparison
Created with Highcharts 8.0.0Total River Discharge (cfs)1. Jan1. Feb1. Mar1. Apr1. May1. Jun1. Jul1. Aug1. Sep1. Oct1. Nov1. Dec1. Jan020k40k
Maximum Streamflow Discharge
Created with Highcharts 8.0.0YearAnnual Peak Discharge(cfs)2010201120122013201420152016201720182019202020212022202320242025202610k20k40k100k

Weather Forecast

Created with Highcharts 8.0.0humidity
Streamflow Elevation Profile
Created with Highcharts 8.0.0

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.

Regional Streamflow Levels