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2025-12-17T18:00:00-07:00

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Whitewater River River Levels

Last Updated: December 17, 2025

The Whitewater River is a 30-mile-long tributary of the Little Miami River in southwestern Ohio.


Summary

Total streamflow across the Whitewater River was last observed at 1,197 cfs, and is expected to yield approximately 2,373 acre-ft of water today; about 60% of normal. River levels are low and may signify a drought. Average streamflow for this time of year is 2,006 cfs, with recent peaks last observed on 2019-02-08 when daily discharge volume was observed at 51,883 cfs.

Maximum discharge along the river is currently at the Whitewater R A Windy Point Main Channel Ca reporting a streamflow rate of 486 cfs. However, the streamgauge with the highest stage along the river is the Whitewater R A Windy Point Overflow Channel Ca with a gauge stage of 12 ft. This river is monitored from 9 different streamgauging stations along the Whitewater River, the highest being situated at an altitude of 1,242 ft, the Whitewater R At Towanda.

River Details

Last Updated 2025-12-17
Discharge Volume 2,373 ACRE-FT
Streamflow 1,196.5 cfs
+5.9 cfs (+0.5%)
Percent of Normal 59.64%
Maximum 51,882.7 cfs
2019-02-08
Seasonal Avg 2,006 cfs
       
River Streamflow Levels
Streamgauge Streamflow Gauge Stage 24hr Change (%) % Normal Minimum (cfs) Maximum (cfs) Air Temp Elevation
Whitewater R At Towanda
USGS 07147070
47 cfs 1.97 ft 3.77
Whitewater River Near Economy
USGS 03274650
1 cfs 4.22 ft 34.29
Whitewater R A Windy Point Overflow Channel Ca
USGS 10257549
0 cfs 12 ft None
Whitewater R A Windy Point Main Channel Ca
USGS 10257548
486 cfs 5.48 ft 0.83
Whitewater River Near Alpine
USGS 03275000
122 cfs 4.43 ft -6.87
Whitewater River At Brookville
USGS 03276500
476 cfs 2.65 ft 2.15
Whitewater R A Rancho Mirage Ca
USGS 10259100
0 cfs 6.36 ft None
Whitewater R A Indio Ca
USGS 10259300
0 cfs 6.62 ft None
Whitewater R Nr Mecca
USGS 10259540
66 cfs 3.46 ft -1.2
Seasonal Discharge Comparison
Maximum Streamflow Discharge
Streamflow Elevation Profile

A whitewater river is classified based on its chemistry, sediments and water colour. Whitewater rivers have high levels of suspended sediments, giving the water a pH that is near-neutral, a high electric conductivity and a pale muddy, café au lait-like colour. Whitewater rivers are of great ecological importance and are important to local fisheries. The major seasonal Amazonian floodplains known as várzea receive their water from them.The best-known whitewater rivers are Amazonian and have their source in the Andes, but there are also whitewater rivers elsewhere in South America and in other continents.Amazonian rivers fall into three main categories: whitewater, blackwater and clearwater. This classification system was first proposed by Alfred Russel Wallace in 1853 based on water colour, but the types were more clearly defined according to chemistry and physics by Harald Sioli (de) from the 1950s to the 1980s. Although many Amazonian rivers fall clearly into one of these categories, others show a mix of characteristics and may vary depending on season and flood levels.