The monitoring network within this area

Hydrionis holds 2,246 values from 4 gauges within it. Discharge is a property of a gauge and its reach, not of this drainage area, so this page reports the network and its records rather than a single figure.

4
Gauges
2,246
Values held
1908–2026
Record spans
Gauges within the Clackamas huc8 subbasin
4 monitoring points, positioned as the publisher records them.
Gauges within the Clackamas huc8 subbasinOAK GROVE FORK ABOVE POWERPLANT INTAKE, OR., CLACKAMAS RIVER ABOVE THREE LYNX CREEK, OR, CLACKAMAS RIVER AT ESTACADA, OR, CLACKAMAS RIVER AT BIG BOTTOM, OROAK GROVE FORK ABOVE POWERPLANT INTAKE, OR.CLACKAMAS RIVER ABOVE THREE LYNX CREEK, ORCLACKAMAS RIVER AT ESTACADA, ORCLACKAMAS RIVER AT BIG BOTTOM, OR

Flood peaks, as measured

This gauge's flood record, as measured. Unlike a daily mean it is the discharge at the moment the river was highest, which is the figure flood frequency analysis is built on.

Largest measured flow of each year at CLACKAMAS RIVER AT ESTACADA, OR
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1909–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at CLACKAMAS RIVER AT ESTACADA, ORLargest measured flow of each year at CLACKAMAS RIVER AT ESTACADA, OR: CLACKAMAS RIVER AT ESTACADA, OR in m³/s, from 1909 to 2025.Hurricane Katrina water and sanitation collapse01,0002,000m³/s19091926194219581971198920032020

Published by the gauge's own operator from its sub-daily record; Hydrionis stores the figure rather than recomputing it. A year the gauge did not cover produces no value rather than a low one, and the gaps are stated below the chart. A peak is a property of this gauge and its reach: a larger flood upstream or downstream of it is not in this series.

What the shaded periods are (1 event)

A shaded period marks when something was recorded, not what caused the shape of the line. Where the two coincide, they coincided.

Documented record — A documented event, compiled from cited sources after it happened. The dates are as good as the record, which for older events can mean the month rather than the day.

EventTypePeriodStandingAuthority
Hurricane Katrina water and sanitation collapseFlood2005-08-29 – 2005-09-30Documented record
Compiled record

Not shown on this chart

  • The 1976 drought — This event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • The 2022 drought — This event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • Yorkshire drought — This event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • Cantareira water crisis, São Paulo — This event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • Cape Town Day Zero — This event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • European drought — This event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
View the data behind this chart
Underlying data
PeriodCLACKAMAS RIVER AT ESTACADA, OR (m³/s)
1909790
1910379
1912677
1913586
1914408
1915187
1917262
1919674
1920847
19211,254
19231,699
1924807
1926620
1927847
1929289
19311,722
1932711
1933518
1934442
1936685
1937663
1939340
1940538
1941651
19421,206
1943259
1945575
19461,303
19481,512
1949705
1950668
1951411
19531,152
1954408
19551,206
1957745
1958660
1959527
1960510
1961651
1962750
1963496
19642,461
1966479
1967671
1968841
1969767
19701,022
1971946
19721,818
19741,699
1975702
1977155
1979586
1980844
19821,206
1983951
1984524
19861,226
1987985
1989648
1990699
1991476
1992524
1994408
1995736
19961,951
1997963
1998977
19991,019
2001198
2002648
2003643
2005436
20061,011
2007702
20091,031
2010436
20111,237
2012824
2014535
2015861
2017617
2019835
2020337
2021878
2022549
2024459
2025566

About this series

Everything below is a property of the data rather than a rating of it. There is deliberately no single confidence score: how much a gap matters depends on what you are about to do with the series, and only you know that.

Source
United States Geological Survey — National Water Information System · US Government work — public domain
How the values came to existMeasured
Period held1909–2025
Completeness76.1% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 28 separate periods inside 1909–2025 hold no value. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1909 and is not continuous from it: 117 years separate the first value from the last, and 76% of the years between them are held. The span is not the record.
Last read from the publisher2026-10-01
RedistributionPermitted by the upstream licences
Commercial reusePermitted by the upstream licences. No Hydrionis access tier can widen this.
MethodologyHow this was produced

How much of the rain came back out

A discharge in cubic metres per second cannot be compared with anything: the larger number may only mean the larger catchment. Divided by the area draining to the gauge it becomes a depth of water over that land, which answers a question a reader already has — of the rain that fell here, how much came back out as river?

Water leaving the catchment above CLACKAMAS RIVER AT ESTACADA, OR, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1909–2024.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above CLACKAMAS RIVER AT ESTACADA, OR, as a depthWater leaving the catchment above CLACKAMAS RIVER AT ESTACADA, OR, as a depth: CLACKAMAS RIVER AT ESTACADA, OR in mm, from 1909 to 2024.Hurricane Katrina water and sanitation collapse5001,0001,5002,0002,500mm19091924193919541969198419992014

Computed by Hydrionis from the published annual mean flow and the catchment area the station's own publisher states. It is not a water balance: the difference between rainfall and runoff is not evaporation alone but also change in groundwater storage, water abstracted and taken elsewhere, and water imported by transfer schemes — which is why a catchment can yield more runoff than the rain that fell on it without anything being measured wrongly. A different area figure rescales every value here by the ratio between them.

What the shaded periods are (1 event)

A shaded period marks when something was recorded, not what caused the shape of the line. Where the two coincide, they coincided.

Documented record — A documented event, compiled from cited sources after it happened. The dates are as good as the record, which for older events can mean the month rather than the day.

EventTypePeriodStandingAuthority
Hurricane Katrina water and sanitation collapseFlood2005-08-29 – 2005-09-30Documented record
Compiled record

Not shown on this chart

  • The 1976 drought — This event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • The 2022 drought — This event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • Yorkshire drought — This event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • Cantareira water crisis, São Paulo — This event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • Cape Town Day Zero — This event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • European drought — This event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
View the data behind this chart
Underlying data
PeriodCLACKAMAS RIVER AT ESTACADA, OR (mm)
19091,661
19101,315
19111,084
19121,464
19131,331
19141,184
19151,186
19161,760
19171,775
19181,347
19191,561
19201,360
19211,944
19221,098
19231,533
19241,122
19251,282
19261,010
19271,589
19281,223
19291,090
1930883
19311,029
19321,438
19331,672
19341,220
19351,056
19361,225
19371,588
19381,370
19391,046
19401,142
19411,000
19421,309
19431,511
1944780
19451,438
19461,646
19471,355
19481,581
19491,528
19502,078
19511,642
19521,144
19531,903
19541,513
19551,836
19561,592
19571,382
19581,467
19591,375
19601,514
19611,623
19621,423
19631,234
19641,646
19651,237
19661,343
19671,232
19681,569
19691,533
19701,533
19711,944
19721,986
19731,377
19741,933
19751,711
19761,273
19771,265
19781,066
19791,219
19801,398
19811,301
19821,680
19831,691
19841,717
19851,202
19861,476
19871,000
19881,321
19891,176
19901,345
19911,325
1992965
19931,234
19941,182
19951,831
19962,136
19971,728
19981,558
19991,724
20001,241
2001981
20021,265
20031,295
20041,240
20051,037
20061,693
20071,333
20081,523
20091,451
20101,523
20111,546
20121,879
20131,229
20141,576
20151,094
20161,336
20171,772
20181,166
20191,041
20201,119
20211,194
20221,555
20231,117
20241,423

About this series

Everything below is a property of the data rather than a rating of it. There is deliberately no single confidence score: how much a gap matters depends on what you are about to do with the series, and only you know that.

Source
United States Geological Survey — National Water Information System · US Government work — public domain
How the values came to existDerived Computed by Hydrionis
Period held1909–2024
Completeness100.0% of the periods in that span are held.
ContinuityContinuous: every year from 1909 to 2024 is held.
Inputs last read2026-10-01 · when the records this was computed from were last read from their publishers
Calculation date2026-08-24 · when the calculation method was last versioned, not a reading of any publisher
RedistributionPermitted by the upstream licences
Commercial reusePermitted by the upstream licences. No Hydrionis access tier can widen this.
MethodologyHow this was produced

The snow standing above this water

2 automated snow stations sit inside this drainage area, weighing the snowpack rather than measuring how deep it is.

543
Fullest snowpack recorded at Clackamas Lake, in 2008 (mm of water)
32
Thinnest, in 2015 (mm of water)
March
Month the pack is usually at its fullest
May
Month the pack has gone by, in half of years
Peak snowpack at Clackamas Lake
Water years 1981–2026. Each point is the fullest month of that snow season.
Peak snowpack at Clackamas LakePeak snowpack at Clackamas Lake: Clackamas Lake in mm, from 1981 to 2026.0200400600mm19811987199319992005201120172023Clackamas Lake 1981: 81.0 mmClackamas Lake 1982: 366 mmClackamas Lake 1983: 252 mmClackamas Lake 1984: 293 mmClackamas Lake 1985: 525 mmClackamas Lake 1986: 359 mmClackamas Lake 1987: 328 mmClackamas Lake 1988: 293 mmClackamas Lake 1989: 417 mmClackamas Lake 1990: 323 mmClackamas Lake 1991: 126 mmClackamas Lake 1992: 63.0 mmClackamas Lake 1993: 426 mmClackamas Lake 1994: 183 mmClackamas Lake 1995: 261 mmClackamas Lake 1996: 122 mmClackamas Lake 1997: 514 mmClackamas Lake 1998: 288 mmClackamas Lake 1999: 369 mmClackamas Lake 2000: 426 mmClackamas Lake 2001: 174 mmClackamas Lake 2002: 458 mmClackamas Lake 2003: 73.0 mmClackamas Lake 2004: 306 mmClackamas Lake 2005: 85.0 mmClackamas Lake 2006: 402 mmClackamas Lake 2007: 237 mmClackamas Lake 2008: 543 mmClackamas Lake 2009: 399 mmClackamas Lake 2010: 125 mmClackamas Lake 2011: 272 mmClackamas Lake 2012: 322 mmClackamas Lake 2013: 231 mmClackamas Lake 2014: 137 mmClackamas Lake 2015: 32.0 mmClackamas Lake 2016: 229 mmClackamas Lake 2017: 409 mmClackamas Lake 2018: 212 mmClackamas Lake 2019: 351 mmClackamas Lake 2020: 275 mmClackamas Lake 2021: 341 mmClackamas Lake 2022: 370 mmClackamas Lake 2023: 401 mmClackamas Lake 2024: 321 mmClackamas Lake 2025: 226 mmClackamas Lake 2026: 81.0 mm

A water year runs October to September and is named for the year it ends, so the snow of one winter stays in one point. The value is the fullest month, not the fullest day: a pack that peaked sharply mid-month reads lower here than a single measurement taken at the right moment would.

View the data behind this chart
Underlying data
PeriodClackamas Lake (mm)
198181.0
1982366
1983252
1984293
1985525
1986359
1987328
1988293
1989417
1990323
1991126
199263.0
1993426
1994183
1995261
1996122
1997514
1998288
1999369
2000426
2001174
2002458
200373.0
2004306
200585.0
2006402
2007237
2008543
2009399
2010125
2011272
2012322
2013231
2014137
201532.0
2016229
2017409
2018212
2019351
2020275
2021341
2022370
2023401
2024321
2025226
202681.0

Why the snow is not read against the river here

OAK GROVE FORK ABOVE POWERPLANT INTAKE, OR. measures a powerplant intake, not a natural channel. What passes through it is an operating decision — how much was diverted, and when — so comparing it with what the sky or the mountain delivered would describe the operator rather than the hydrology.

Every gauge Hydrionis holds within this area

Gauges within the Clackamas and what each holds
GaugeMeasuresValuesRecord
CLACKAMAS RIVER AT ESTACADA, ORburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3871908–2026
OAK GROVE FORK ABOVE POWERPLANT INTAKE, OR.burned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3601909–2026
CLACKAMAS RIVER ABOVE THREE LYNX CREEK, ORburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3561909–2026
CLACKAMAS RIVER AT BIG BOTTOM, ORcatchment area, annual maximum river flow511921–2026

How these gauges were attached to this water

Assigned by the publisher to a numbered basin Every gauge here is assigned to this drainage area by its own publisher, which issues the area an official code — 17090011. A drainage area is not a river: it contains the tributaries as well as the main channel, and a gauge in it may be on any of them.

What each gauge’s link to this water rests on
GaugeEvidenceEstablished
CLACKAMAS RIVER AT ESTACADA, ORStated by the publisher — USGS site service, huc_cd field — https://waterservices.usgs.gov/nwis/site/ ; named from the USGS Watershed Boundary Dataset 8-digit HU (Subbasin) layer — https://hydro.nationalmap.gov/arcgis/rest/services/wbd/MapServer/42026-10-02
OAK GROVE FORK ABOVE POWERPLANT INTAKE, OR.Stated by the publisher — USGS site service, huc_cd field — https://waterservices.usgs.gov/nwis/site/ ; named from the USGS Watershed Boundary Dataset 8-digit HU (Subbasin) layer — https://hydro.nationalmap.gov/arcgis/rest/services/wbd/MapServer/42026-10-02
CLACKAMAS RIVER ABOVE THREE LYNX CREEK, ORStated by the publisher — USGS site service, huc_cd field — https://waterservices.usgs.gov/nwis/site/ ; named from the USGS Watershed Boundary Dataset 8-digit HU (Subbasin) layer — https://hydro.nationalmap.gov/arcgis/rest/services/wbd/MapServer/42026-10-02
CLACKAMAS RIVER AT BIG BOTTOM, ORStated by the publisher — USGS site service, huc_cd field — https://waterservices.usgs.gov/nwis/site/ ; named from the USGS Watershed Boundary Dataset 8-digit HU (Subbasin) layer — https://hydro.nationalmap.gov/arcgis/rest/services/wbd/MapServer/42026-10-02

What this record holds

Hydrionis decides which waters get a page, and which of those are offered to search, from what is actually held rather than from how the page reads. Five signals are counted; this record has 5 of them, which makes it a full profile.

Information-gain signals held for this water body
SignalHeldCounts
Gauges holding a real record4yes, 3 or more
Years spanned119yes, 20 or more
Values held2,246yes, 1000 or more
Distinct measurements6yes, 2 or more
Publishers measuring it2yes, 2 or more
Official identifiers1recorded, not counted

Use this data

Use this data

No bulk download is offered here, which is a licence position rather than a product one: at least one contributing publisher does not permit redistribution. The values can be read on the page, cited, and pointed to at source.

Attribution and citation

Suggested citation for Hydrionis

Hydrionis (2026), Clackamas gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-clackamas/

Cite Hydrionis where you rely on values Hydrionis computed, on the method that produced them, or on the compilation itself. The underlying measurements remain the publishers’ and their attribution requirements apply to you directly.

Recommended, not required. Hydrionis does not claim rights over unmodified public data it relayed, and doing arithmetic on somebody else’s measurements does not make them Hydrionis’s. Cite the version and the access date: the Clackamas gauge records changes as publishers release and as methods are revised, and a citation without both cannot be checked later. Full guidance is on cite and reuse.

None of the contributing licences requires attribution. Crediting the publishers is still good practice and they are listed above.

Where these figures come from

MeasuredHigh confidence2025-02-23

Source: USGS — National Water Information System, USGS site 14210000, annual peak streamflow. Licence: Open.

Method: The instantaneous maximum discharge of each water year as published by USGS, dated to the day it occurred. One value per October-to-September water year; where the publisher lists both a systematic and a historic peak for a year, the larger is the annual maximum. Values the publisher marks as maximum daily averages are not held here, because they are not instantaneous peaks. Values marked as bounded rather than measured are held as censored observations carrying the bound. Cubic feet per second are converted to cubic metres per second and the publisher unit is recorded alongside.

Rating curves are extrapolated at extreme discharges, so the largest values in a peak series carry the largest measurement uncertainty. Data from the U.S. Geological Survey National Water Information System, a work of the United States government and therefore in the public domain.

Retrieved 1 October 2026.