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 |
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 |
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.