Streamflow

Below normal

Willamette River at Portland streamflow

Daily mean discharge, Willamette-Columbia basin, Oregon

Data through Sep 29, 2026 · source last checked Oct 1, 2026 · page revised Oct 1, 2026

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About this data
Source
US Geological Survey (USGS)
Series
Daily mean streamflow (discharge)
Geography
Willamette River at Portland
Unit
cfs
Calculation
Daily mean
Last observation
Sep 29, 2026
Update frequency
Daily

Now 6,580 cfs, 17% below the 5-yr median.

Willamette flow at Portland fell to 6,580 cfs, down 21.7% on the week. Month-over-month the gauge has recovered 23.0%, but it remains 17% below the 5-year median.

The numbers
PeriodCurrentPriorChange
Week over week6,580 cfs8,400 cfs-21.7%
Month over month6,580 cfs5,350 cfs+23.0%
Year over year6,580 cfs7,800 cfs-15.6%
vs 5-yr median6,580 cfs7,890 cfs-16.6%
Typical flow for this week of the year (5-year record)
ReadingDischarge
Lowest on record for this week6,200 cfs
Median for this week7,890 cfs
Highest on record for this week13,900 cfs

Previous weeks

Week of Sep 23, 2026

Willamette flow at Portland fell to 5,490 cfs, down 9.4% on the week and 8.8% on the month. Year-over-year the decline reaches 27.6%, with current flow 28% below the 5-year median of 7,580 cfs.

Week of Sep 15, 2026

Flow at the Willamette River gauge dropped to 6,710 cfs, down 25.4% on the week. Discharge has risen 26.6% from a month ago but runs 2% below the 5-year median.

Week of Sep 2, 2026

Willamette discharge at Portland is 6,200 cfs, 20% below the 5-yr median. Flow fell 11.4% week-over-week but has recovered 59% from a month ago. Year-over-year the gauge is down 22.9%.

Week of Aug 26, 2026

Willamette discharge jumped to 7,000 cfs, up 47.7% on the week, though down 13.4% since last month. The river runs 9% above its 5-year median.

About Willamette River at Portland

USGS gage 14211720 sits on the Willamette River at Portland, at the Morrison Bridge, near the bottom of a valley that drains about 11,200 square miles between the Cascades and the Coast Range. Thirteen federal dams sit on its tributaries, operated by the Corps of Engineers for winter flood control and for summer flow augmentation in the mainstem.

The Willamette is a rain river rather than a snowmelt river, so a normal year is dominated by winter storm peaks between November and March and settles into a low, stable, largely reservoir-supported summer. Storm peaks arrive and pass within days. The gage sits close enough to the Columbia that its record is tidally influenced at low flow, which is worth knowing before reading small day-to-day movements as hydrology. Low summer readings are the ones that matter locally, for temperature and dissolved oxygen in the reach through the city and for the fish using it.