SNOFLO



FRASER RIVER

RIVER LEVELS
April 28, 2025


Total streamflow across the Fraser River was last observed at 32 cfs, and is expected to yield approximately 64 acre-ft of water today; about 50% of normal. River levels are low and may signify a drought. Average streamflow for this time of year is 64 cfs, with recent peaks last observed on 2014-05-31 when daily discharge volume was observed at 2,549 cfs.

Maximum discharge along the river is currently at the Fraser River Blw Crooked Cr At Tabernash Co reporting a streamflow rate of 30.4 cfs. This is also the highest stage along the Fraser River, with a gauge stage of 2.67 ft at this location. This river is monitored from 3 different streamgauging stations along the Fraser River, the highest being situated at an altitude of 9,539 ft, the Fraser River At Upper Sta.

Last Updated 2025-04-28
Discharge Volume 64 ACRE-FT
Streamflow 32.1 cfs
+2.0 cfs (+6.64%)
Percent of Normal 50.01%
Maximum 2,549.0 cfs
2014-05-31
Seasonal Avg 64 cfs
       
River Streamflow Levels
Created with Highcharts 8.0.0Total River Discharge (cfs)19. Apr20. Apr21. Apr22. Apr23. Apr24. Apr25. Apr26. Apr27. Apr28. Apr02040
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. Jan050010001500
Maximum Streamflow Discharge
Created with Highcharts 8.0.0YearAnnual Peak Discharge(cfs)20102011201220132014201520162017201820192020202120222023202420252026101001k10k

Weather Forecast

Streamflow Elevation Profile
Created with Highcharts 8.0.0

The Fraser River is the longest river within British Columbia, Canada, rising at Fraser Pass near Blackrock Mountain in the Rocky Mountains and flowing for 1,375 kilometres (854 mi), into the Strait of Georgia at the city of Vancouver. It is the 11th longest river in Canada. The river's annual discharge at its mouth is 112 cubic kilometres (27 cu mi) or 3,550 cubic metres per second (125,000 cu ft/s), and it discharges 20 million tons of sediment into the ocean.