SNOFLO
 



PALOUSE RIVER

RIVER LEVELS
April 28, 2025


Total streamflow across the Palouse River was last observed at 535 cfs, and is expected to yield approximately 1,061 acre-ft of water today; about 37% of normal. River levels are low and may signify a drought. Average streamflow for this time of year is 1,465 cfs, with recent peaks last observed on 2012-04-01 when daily discharge volume was observed at 15,260 cfs.

Maximum discharge along the river is currently at the Palouse River At Hooper reporting a streamflow rate of 424 cfs. However, the streamgauge with the highest stage along the river is the Palouse River Nr Potlatch Id with a gauge stage of 6.21 ft. This river is monitored from 2 different streamgauging stations along the Palouse River, the highest being situated at an altitude of 2,481 ft, the Palouse River Nr Potlatch Id.

Last Updated 2025-04-28
Discharge Volume 1,061 ACRE-FT
Streamflow 535.0 cfs
-29.0 cfs (-5.14%)
Percent of Normal 36.52%
Maximum 15,260.0 cfs
2012-04-01
Seasonal Avg 1,465 cfs
       
River Streamflow Levels
Created with Highcharts 8.0.0Total River Discharge (cfs)19. Apr20. Apr21. Apr22. Apr23. Apr24. Apr25. Apr26. Apr27. Apr28. Apr05001000
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

Streamflow Elevation Profile
Created with Highcharts 8.0.0

The Palouse River is a tributary of the Snake River in Washington and Idaho, in the northwest United States. It flows for 167 miles (269 km) southwestwards, primarily through the Palouse region of southeastern Washington. It is part of the Columbia River Basin, as the Snake River is a tributary of the Columbia River.
Its canyon was carved out by a fork in the catastrophic Missoula Floods of the previous ice age, which spilled over the northern Columbia Plateau and flowed into the Snake River, eroding the river's present course in a few thousand years.