The monitoring network within this area

Hydrionis holds 3,432 values from 12 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.

12
Gauges
3,432
Values held
1906–2026
Record spans
Gauges within the Upper Deschutes huc8 subbasin
12 monitoring points, positioned as the publisher records them.
Gauges within the Upper Deschutes huc8 subbasinCULTUS RIVER AB CULTUS CR NR LA PINE,OREG., CULTUS CR AB CRANE PRAIRIE RES NR LA PINE,OREG., DEER CR AB CRANE PRAIRIE RES NR LA PINE,OREG., DESCHUTES R BL CRANE PRAIRIE RES NR LA PINE, OR, DESCHUTES R AT BENHAM FALLS NR BEND, OR, TUMALO CREEK PLUS COL SO CA, NR TUMALA, OR, WHYCHUS CREEK NEAR SISTERS, OR, LAKE CREEK NEAR SISTERS,OREG., METOLIUS RIVER NEAR GRANDVIEW, OR, BROWN CREEK NEAR LA PINE,OREG., ODELL CREEK NEAR CRESCENT,OREG., DESCHUTES RIVER BELOW BEND,OREG.CULTUS RIVER AB CULTUS CR NR LA PINE,OREG.CULTUS CR AB CRANE PRAIRIE RES NR LA PINE,OREG.DEER CR AB CRANE PRAIRIE RES NR LA PINE,OREG.DESCHUTES R BL CRANE PRAIRIE RES NR LA PINE, ORDESCHUTES R AT BENHAM FALLS NR BEND, ORTUMALO CREEK PLUS COL SO CA, NR TUMALA, ORWHYCHUS CREEK NEAR SISTERS, ORLAKE CREEK NEAR SISTERS,OREG.METOLIUS RIVER NEAR GRANDVIEW, ORBROWN CREEK NEAR LA PINE,OREG.ODELL CREEK NEAR CRESCENT,OREG.DESCHUTES RIVER BELOW BEND,OREG.

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 METOLIUS RIVER NEAR GRANDVIEW, OR
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1913–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at METOLIUS RIVER NEAR GRANDVIEW, ORLargest measured flow of each year at METOLIUS RIVER NEAR GRANDVIEW, OR: METOLIUS RIVER NEAR GRANDVIEW, OR in m³/s, from 1913 to 2025.Hurricane Katrina water and sanitation collapse0100200m³/s19131933194819611975198920012015

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
PeriodMETOLIUS RIVER NEAR GRANDVIEW, OR (m³/s)
191358.6
1921119
1923164
192583.0
192662.3
1927110
192848.7
192948.7
193183.0
193254.7
193378.7
193462.3
193652.7
193758.3
193851.0
194046.4
194140.2
1943145
194554.4
194687.2
194885.5
194962.3
195063.4
195178.4
195258.9
195395.1
195563.1
195681.3
195871.6
196058.6
1961110
196386.1
1964213
196652.1
196753.8
196881.6
197082.7
197191.2
1972101
1974124
197570.2
197745.6
197855.2
198069.7
1982152
198379.9
198473.6
198564.3
1986126
198750.1
198949.6
199072.8
199154.9
199368.2
199442.2
199583.3
1996239
1997146
199893.2
1999125
200156.1
200279.6
200378.2
200455.5
2006110
200875.3
201070.8
2011112
201285.8
201499.4
201569.7
201781.3
2019109
202051.3
202181.0
202283.0
202364.8
202573.1

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 held1913–2025
Completeness69.0% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 29 separate periods inside 1913–2025 hold no value. The longest runs from 1914 to 1920 — 7 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1913 and is not continuous from it: 113 years separate the first value from the last, and 69% 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 METOLIUS RIVER NEAR GRANDVIEW, 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. 1913–2024.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above METOLIUS RIVER NEAR GRANDVIEW, OR, as a depthWater leaving the catchment above METOLIUS RIVER NEAR GRANDVIEW, OR, as a depth: METOLIUS RIVER NEAR GRANDVIEW, OR in mm, from 1913 to 2024.Hurricane Katrina water and sanitation collapse1,2501,5001,7502,000mm19131934194719601973198619992012

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
PeriodMETOLIUS RIVER NEAR GRANDVIEW, OR (mm)
19131,750
19221,687
19231,793
19241,562
19251,737
19261,535
19271,748
19281,668
19291,487
19301,439
19311,318
19321,489
19331,555
19341,585
19351,564
19361,514
19371,506
19381,620
19391,400
19401,354
19411,282
19421,355
19431,652
19441,312
19451,368
19461,518
19471,465
19481,559
19491,633
19501,856
19511,890
19521,794
19531,909
19541,865
19551,747
19561,980
19571,759
19581,834
19591,667
19601,647
19611,740
19621,664
19631,583
19641,648
19651,787
19661,591
19671,553
19681,580
19691,654
19701,616
19711,794
19722,004
19731,613
19741,904
19751,825
19761,810
19771,520
19781,492
19791,418
19801,520
19811,538
19821,820
19831,837
19841,766
19851,581
19861,673
19871,473
19881,487
19891,502
19901,470
19911,415
19921,365
19931,498
19941,336
19951,588
19961,999
19972,100
19981,799
19992,052
20001,865
20011,535
20021,632
20031,532
20041,600
20051,412
20061,740
20071,645
20081,745
20091,752
20101,687
20111,859
20121,953
20131,700
20141,866
20151,651
20161,673
20171,807
20181,613
20191,634
20201,509
20211,490
20221,586
20231,472
20241,556

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 held1913–2024
Completeness92.9% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • One period inside 1913–2024 holds no value: 1914 to 1921, 8 years with no reading. It is drawn as a break in the line and is never interpolated across.
ContinuityThe record begins in 1913 and is not continuous from it: 112 years separate the first value from the last, and 93% of the years between them are held. The span is not the record.
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.

1,670
Fullest snowpack recorded at Irish Taylor, in 1999 (mm of water)
236
Thinnest, in 2026 (mm of water)
April
Month the pack is usually at its fullest
July
Month the pack has gone by, in half of years
Peak snowpack at Irish Taylor
Water years 1979–2026. Each point is the fullest month of that snow season.
Peak snowpack at Irish TaylorPeak snowpack at Irish Taylor: Irish Taylor in mm, from 1979 to 2026.05001,0001,5002,000mm19791985199119972003200920152021Irish Taylor 1979: 598 mmIrish Taylor 1980: 780 mmIrish Taylor 1981: 515 mmIrish Taylor 1982: 1,288 mmIrish Taylor 1983: 1,087 mmIrish Taylor 1984: 1,318 mmIrish Taylor 1985: 1,207 mmIrish Taylor 1986: 1,035 mmIrish Taylor 1987: 873 mmIrish Taylor 1988: 840 mmIrish Taylor 1989: 1,230 mmIrish Taylor 1990: 363 mmIrish Taylor 1991: 550 mmIrish Taylor 1992: 324 mmIrish Taylor 1993: 1,267 mmIrish Taylor 1994: 628 mmIrish Taylor 1995: 1,004 mmIrish Taylor 1996: 912 mmIrish Taylor 1997: 1,211 mmIrish Taylor 1998: 789 mmIrish Taylor 1999: 1,670 mmIrish Taylor 2000: 1,043 mmIrish Taylor 2001: 504 mmIrish Taylor 2002: 1,121 mmIrish Taylor 2003: 783 mmIrish Taylor 2004: 1,186 mmIrish Taylor 2005: 681 mmIrish Taylor 2006: 1,171 mmIrish Taylor 2007: 823 mmIrish Taylor 2008: 1,263 mmIrish Taylor 2009: 1,030 mmIrish Taylor 2010: 806 mmIrish Taylor 2011: 1,061 mmIrish Taylor 2012: 962 mmIrish Taylor 2013: 691 mmIrish Taylor 2014: 701 mmIrish Taylor 2015: 249 mmIrish Taylor 2016: 875 mmIrish Taylor 2017: 998 mmIrish Taylor 2018: 586 mmIrish Taylor 2019: 780 mmIrish Taylor 2020: 670 mmIrish Taylor 2021: 841 mmIrish Taylor 2022: 746 mmIrish Taylor 2024: 981 mmIrish Taylor 2025: 1,059 mmIrish Taylor 2026: 236 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
PeriodIrish Taylor (mm)
1979598
1980780
1981515
19821,288
19831,087
19841,318
19851,207
19861,035
1987873
1988840
19891,230
1990363
1991550
1992324
19931,267
1994628
19951,004
1996912
19971,211
1998789
19991,670
20001,043
2001504
20021,121
2003783
20041,186
2005681
20061,171
2007823
20081,263
20091,030
2010806
20111,061
2012962
2013691
2014701
2015249
2016875
2017998
2018586
2019780
2020670
2021841
2022746
2024981
20251,059
2026236

Read against the river

Irish Taylor and CULTUS RIVER AB CULTUS CR NR LA PINE,OREG. both sit in this drainage area, and their records overlap by 11 years. That is the span the two have in common, not a count of years both actually hold — either record may have gaps inside it. The two are shown separately rather than on one axis: millimetres of stored water and cubic metres per second are not commensurable, and a difference between them would mean nothing.

Being in the same drainage area does not put the snowpack upstream of the gauge. A subbasin is an area, and snow on one tributary can join the river below a gauge on another — so a weak relationship here may say more about which tributary was measured than about the snow.

Every gauge Hydrionis holds within this area

Gauges within the Upper Deschutes and what each holds
GaugeMeasuresValuesRecord
METOLIUS RIVER NEAR GRANDVIEW, ORburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3501912–2026
WHYCHUS CREEK NEAR SISTERS, ORburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2741906–2026
LAKE CREEK NEAR SISTERS,OREG.burned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2541915–2026
DESCHUTES R BL CRANE PRAIRIE RES NR LA PINE, ORburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2461914–2026
DESCHUTES R AT BENHAM FALLS NR BEND, ORburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2361907–2026
CULTUS CR AB CRANE PRAIRIE RES NR LA PINE,OREG.burned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year1981924–2026
DEER CR AB CRANE PRAIRIE RES NR LA PINE,OREG.burned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year1971924–2026
TUMALO CREEK PLUS COL SO CA, NR TUMALA, ORburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year1931923–2026
CULTUS RIVER AB CULTUS CR NR LA PINE,OREG.burned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year1911923–2026
DESCHUTES RIVER BELOW BEND,OREG.catchment area, annual maximum river flow771915–2026
BROWN CREEK NEAR LA PINE,OREG.catchment area, annual maximum river flow521923–2026
ODELL CREEK NEAR CRESCENT,OREG.catchment area, annual maximum river flow451933–2026

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 — 17070301. 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
METOLIUS RIVER NEAR GRANDVIEW, 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
WHYCHUS CREEK NEAR SISTERS, 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
LAKE CREEK NEAR SISTERS,OREG.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
DESCHUTES R BL CRANE PRAIRIE RES NR LA PINE, 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
DESCHUTES R AT BENHAM FALLS NR BEND, 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
CULTUS CR AB CRANE PRAIRIE RES NR LA PINE,OREG.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
DEER CR AB CRANE PRAIRIE RES NR LA PINE,OREG.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
TUMALO CREEK PLUS COL SO CA, NR TUMALA, 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
CULTUS RIVER AB CULTUS CR NR LA PINE,OREG.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
DESCHUTES RIVER BELOW BEND,OREG.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
BROWN CREEK NEAR LA PINE,OREG.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
ODELL CREEK NEAR CRESCENT,OREG.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

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 record11yes, 3 or more
Years spanned121yes, 20 or more
Values held3,432yes, 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), Upper Deschutes gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-upper-deschutes/

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 Upper Deschutes 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 14091500, 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.