* WHAT...Snow expected. Total snow accumulations between 3 and 7 inches. * WHERE...Castle Rock. * WHEN...From 3 PM this afternoon to noon MDT Saturday. * IMPACTS...Snow covered roads could make travel hazardous. The hazardous conditions will impact the Friday evening commute.
Total streamflow across the
Clearwater River
was last observed at
79,280
cfs, and is expected to yield approximately
157,250
acre-ft of water today; about 120%
of normal.
Average streamflow for this time of year is
66,139 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 At Spalding Id
reporting a streamflow rate of 31,700 cfs.
However, the streamgauge with the highest stage along the river is the
Clearwater River Nr Peck Id
with a gauge stage of 11.32 ft.
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 | 2025-04-18 |
Discharge Volume | 157,250 ACRE-FT |
Streamflow |
79,280.0 cfs
+10.0 cfs (+0.01%) |
Percent of Normal | 119.87% |
Maximum |
263,553.0 cfs
2022-06-12 |
Seasonal Avg | 66,139 cfs |
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.