CLEARWATER RIVER

RIVER LEVELS
May 14, 2025


Total streamflow across the Clearwater River was last observed at 115,152 cfs, and is expected to yield approximately 228,402 acre-ft of water today; about 116% of normal. Average streamflow for this time of year is 99,047 cfs, with recent peaks last observed on 2022-06-12 when daily discharge volume was observed at 263,553 cfs.

Maximum discharge along the river is currently at the Clearwater River Nr Peck Id reporting a streamflow rate of 37,700 cfs. This is also the highest stage along the Clearwater River, with a gauge stage of 12.7 ft at this location. This river is monitored from 7 different streamgauging stations along the Clearwater River, the highest being situated at an altitude of 3,909 ft, the Clearwater R Ab Trap Cr Nr T Falls.

Last Updated 2025-05-13
Discharge Volume 228,402 ACRE-FT
Streamflow 115,152.2 cfs
+252.0 cfs (+0.22%)
Percent of Normal 116.26%
Maximum 263,553.0 cfs
2022-06-12
Seasonal Avg 99,047 cfs
       
River Streamflow Levels
Streamgauge Streamflow Gauge Stage 24hr Change (%) % Normal Minimum (cfs) Maximum (cfs) Air Temp Elevation
Clearwater R Ab Trap Cr Nr T Falls
USGS 14314500
72 cfs 3.73 ft 2.71
Clearwater R Blw Mowich Creek
USGS 14314700
72 cfs 4.95 ft 1.54
Clearwater River At Plummer
USGS 05078000
106 cfs 3.14 ft -18.93
Clearwater River At Orofino Id
USGS 13340000
36200 cfs 11.81 ft -0.28
Clearwater River At Red Lake Falls
USGS 05078500
322 cfs 6.17 ft -4.87
Clearwater River Nr Peck Id
USGS 13341050
37700 cfs 12.7 ft 0
Clearwater River At Spalding Id
USGS 13342500
35300 cfs 10.18 ft 1
Seasonal Discharge Comparison
Maximum Streamflow Discharge

Weather Forecast

Streamflow Elevation Profile

A clearwater river is classified based on its chemistry, sediments and water colour. Clearwater rivers have a low conductivity, relatively low levels of dissolved solids, typically have a neutral to slightly acidic pH and are very clear with a greenish colour. Clearwater rivers often have fast-flowing sections.The main clearwater rivers are South American and have their source in the Brazilian Plateau or the Guiana Shield. Outside South America the classification is not commonly used, but rivers with clearwater characteristics are found elsewhere.Amazonian rivers fall into three main categories: clearwater, blackwater and whitewater. 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.