SNOFLO



NAUGATUCK RIVER

RIVER LEVELS
April 30, 2025


Total streamflow across the Naugatuck River was last observed at 627 cfs, and is expected to yield approximately 1,244 acre-ft of water today; about 73% of normal. Average streamflow for this time of year is 860 cfs, with recent peaks last observed on 2021-09-02 when daily discharge volume was observed at 14,338 cfs.

Maximum discharge along the river is currently at the Naugatuck River At Beacon Falls reporting a streamflow rate of 440 cfs. However, the streamgauge with the highest stage along the river is the Naugatuck River At Thomaston with a gauge stage of 2.44 ft. This river is monitored from 2 different streamgauging stations along the Naugatuck River, the highest being situated at an altitude of 378 ft, the Naugatuck River At Thomaston.

Last Updated 2025-04-30
Discharge Volume 1,244 ACRE-FT
Streamflow 627.0 cfs
-135.0 cfs (-17.72%)
Percent of Normal 72.87%
Maximum 14,338.0 cfs
2021-09-02
Seasonal Avg 860 cfs
       
River Streamflow Levels
Created with Highcharts 8.0.0Total River Discharge (cfs)21. Apr22. Apr23. Apr24. Apr25. Apr26. Apr27. Apr28. Apr29. Apr30. Apr01k2k
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. Jan05k10k15k
Maximum Streamflow Discharge
Created with Highcharts 8.0.0YearAnnual Peak Discharge(cfs)201020112012201320142015201620172018201920202021202220232024202520262k4k10k20k

Weather Forecast

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

The Naugatuck River is a 40.2-mile-long (64.7 km) river in the U.S. state of Connecticut. Its waters carve out the Naugatuck River Valley in the western reaches of the state, flowing generally due south and eventually emptying into the Housatonic River at Derby, Connecticut and thence 11 miles (18 km) to Long Island Sound. The Plume and Atwood Dam in Thomaston, completed in 1960 following the Great Flood of 1955, creates a reservoir on the river and is the last barrier to salmon and trout migrating up from the sea.

Regional Streamflow Levels