The monitoring network within this area

Hydrionis holds 2,693 values from 7 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.

7
Gauges
2,693
Values held
1904–2026
Record spans
Gauges within the Wallowa huc8 subbasin
7 monitoring points, positioned as the publisher records them.
Gauges within the Wallowa huc8 subbasinEAST FORK WALLOWA RIVER NEAR JOSEPH, OR, EAST FK WALLOWA R & W FLS PP TR NR JOSEPH,OREG., WALLOWA RIVER AT JOSEPH,OREG., HURRICANE CREEK NEAR JOSEPH, OREG., LOSTINE RIVER NEAR LOSTINE, OR, BEAR CREEK NEAR WALLOWA, OR, MINAM RIVER AT MINAM, OREAST FORK WALLOWA RIVER NEAR JOSEPH, OREAST FK WALLOWA R & W FLS PP TR NR JOSEPH,OREG.WALLOWA RIVER AT JOSEPH,OREG.HURRICANE CREEK NEAR JOSEPH, OREG.LOSTINE RIVER NEAR LOSTINE, ORBEAR CREEK NEAR WALLOWA, ORMINAM RIVER AT MINAM, 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 LOSTINE RIVER NEAR LOSTINE, OR
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1913–2012.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at LOSTINE RIVER NEAR LOSTINE, ORLargest measured flow of each year at LOSTINE RIVER NEAR LOSTINE, OR: LOSTINE RIVER NEAR LOSTINE, OR in m³/s, from 1913 to 2012.Hurricane Katrina water and sanitation collapse020406080m³/s19131936194719581969198019912006

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
PeriodLOSTINE RIVER NEAR LOSTINE, OR (m³/s)
191371.9
192618.8
192756.9
192856.9
192944.5
193030.9
193129.4
193251.0
193365.4
193430.6
193532.8
193650.1
193736.5
193852.7
193932.8
194035.1
194127.1
194236.2
194350.4
194433.4
194550.4
194641.9
194742.5
194855.5
194941.9
195049.8
195135.4
195248.1
195345.9
195437.9
195547.9
195653.2
195761.4
195849.3
195950.4
196039.9
196149.3
196244.2
196338.2
196441.9
196551.5
196631.1
196751.5
196837.9
196962.6
197060.9
197164.8
197254.9
197333.1
197472.2
197564.3
197639.1
197734.8
197840.8
197936.2
198038.5
198144.5
198253.5
198349.3
198464.3
198549.6
198660.3
198734.3
198831.4
198950.1
199034.3
199136.8
199654.1
199752.4
199827.7
199954.4
200031.7
200130.6
200247.0
200359.5
200439.6
200530.3
200648.4
200851.8
200946.7
201060.6
201145.6
201242.8

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 held1913–2012
Completeness83.0% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 3 separate periods inside 1913–2012 hold no value. The longest runs from 1914 to 1925 — 12 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: 100 years separate the first value from the last, and 83% 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 LOSTINE RIVER NEAR LOSTINE, 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. 1913–2011.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above LOSTINE RIVER NEAR LOSTINE, OR, as a depthWater leaving the catchment above LOSTINE RIVER NEAR LOSTINE, OR, as a depth: LOSTINE RIVER NEAR LOSTINE, OR in mm, from 1913 to 2011.Hurricane Katrina water and sanitation collapse5007501,0001,250mm19131936194719581969198019962007

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
PeriodLOSTINE RIVER NEAR LOSTINE, OR (mm)
19131,329
1926677
19271,324
19281,002
1929691
1930699
1931603
1932971
1933985
1934816
1935733
1936817
1937695
19381,053
1939700
1940753
1941849
1942870
19431,146
1944672
1945950
19461,173
19471,079
19481,158
1949987
19501,097
1951885
19521,052
19531,056
1954886
1955842
19561,256
19571,050
19581,198
19591,131
1960829
1961920
19621,028
1963786
1964912
19651,243
1966617
19671,030
1968886
1969941
19701,104
19711,193
19721,096
1973703
19741,313
19751,157
1976982
1977525
19781,089
1979783
1980976
1981888
19821,207
1983971
19841,127
1985825
1986888
1987613
1988651
1989851
1990827
19961,166
19971,254
1998845
19991,014
2000855
2001573
2002879
2003844
2004964
2005753
20061,060
2007701
20081,061
2009894
2010862
20111,072

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 held1913–2011
Completeness82.8% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 2 separate periods inside 1913–2011 hold no value. The longest runs from 1914 to 1925 — 12 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: 99 years separate the first value from the last, and 83% 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.

850
Fullest snowpack recorded at Mt. Howard, in 1997 (mm of water)
201
Thinnest, in 1981 (mm of water)
April
Month the pack is usually at its fullest
June
Month the pack has gone by, in half of years
Peak snowpack at Mt. Howard
Water years 1981–2026. Each point is the fullest month of that snow season.
Peak snowpack at Mt. HowardPeak snowpack at Mt. Howard: Mt. Howard in mm, from 1981 to 2026.02505007501,000mm19811987199319992005201120172023Mt. Howard 1981: 201 mmMt. Howard 1982: 710 mmMt. Howard 1983: 269 mmMt. Howard 1984: 671 mmMt. Howard 1985: 307 mmMt. Howard 1986: 574 mmMt. Howard 1987: 354 mmMt. Howard 1988: 411 mmMt. Howard 1989: 527 mmMt. Howard 1990: 378 mmMt. Howard 1991: 541 mmMt. Howard 1992: 220 mmMt. Howard 1993: 404 mmMt. Howard 1994: 239 mmMt. Howard 1995: 515 mmMt. Howard 1996: 435 mmMt. Howard 1997: 850 mmMt. Howard 1998: 456 mmMt. Howard 1999: 500 mmMt. Howard 2000: 472 mmMt. Howard 2001: 340 mmMt. Howard 2002: 474 mmMt. Howard 2003: 569 mmMt. Howard 2004: 328 mmMt. Howard 2005: 381 mmMt. Howard 2006: 567 mmMt. Howard 2007: 315 mmMt. Howard 2008: 567 mmMt. Howard 2009: 559 mmMt. Howard 2010: 426 mmMt. Howard 2011: 476 mmMt. Howard 2012: 565 mmMt. Howard 2013: 399 mmMt. Howard 2014: 577 mmMt. Howard 2015: 335 mmMt. Howard 2016: 363 mmMt. Howard 2017: 589 mmMt. Howard 2018: 406 mmMt. Howard 2019: 530 mmMt. Howard 2020: 392 mmMt. Howard 2021: 314 mmMt. Howard 2022: 514 mmMt. Howard 2023: 488 mmMt. Howard 2024: 399 mmMt. Howard 2025: 404 mmMt. Howard 2026: 242 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
PeriodMt. Howard (mm)
1981201
1982710
1983269
1984671
1985307
1986574
1987354
1988411
1989527
1990378
1991541
1992220
1993404
1994239
1995515
1996435
1997850
1998456
1999500
2000472
2001340
2002474
2003569
2004328
2005381
2006567
2007315
2008567
2009559
2010426
2011476
2012565
2013399
2014577
2015335
2016363
2017589
2018406
2019530
2020392
2021314
2022514
2023488
2024399
2025404
2026242

Read against the river

Mt. Howard and EAST FORK WALLOWA RIVER NEAR JOSEPH, OR both sit in this drainage area, and their records overlap by 44 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 Wallowa and what each holds
GaugeMeasuresValuesRecord
LOSTINE RIVER NEAR LOSTINE, ORburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2871912–2026
BEAR CREEK NEAR WALLOWA, ORburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2701915–2026
WALLOWA RIVER AT JOSEPH,OREG.burned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2341904–2026
MINAM RIVER AT MINAM, ORburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2191912–2026
EAST FK WALLOWA R & W FLS PP TR NR JOSEPH,OREG.burned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2091924–2026
EAST FORK WALLOWA RIVER NEAR JOSEPH, ORburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2041924–2026
HURRICANE CREEK NEAR JOSEPH, OREG.burned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year1991915–2026

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 — 17060105. 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
LOSTINE RIVER NEAR LOSTINE, 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
BEAR CREEK NEAR WALLOWA, 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
WALLOWA RIVER AT JOSEPH,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
MINAM RIVER AT MINAM, 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
EAST FK WALLOWA R & W FLS PP TR NR JOSEPH,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
EAST FORK WALLOWA RIVER NEAR JOSEPH, 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
HURRICANE CREEK NEAR JOSEPH, 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 record7yes, 3 or more
Years spanned123yes, 20 or more
Values held2,693yes, 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), Wallowa gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-wallowa/

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 Wallowa 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 confidence2012-06-05

Source: USGS — National Water Information System, USGS site 13330000, 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.