The monitoring network within this area

Hydrionis holds 2,236 values from 3 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.

3
Gauges
2,236
Values held
1909–2026
Record spans
Gauges within the Bruneau huc8 subbasin
3 monitoring points, positioned as the publisher records them.
Gauges within the Bruneau huc8 subbasinBRUNEAU RIVER NR HOT SPRING ID, BRUNEAU RV AT ROWLAND, NV, EF BRUNEAU RIVER NR HOT SPRING IDBRUNEAU RIVER NR HOT SPRING IDBRUNEAU RV AT ROWLAND, NVEF BRUNEAU RIVER NR HOT SPRING ID

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 BRUNEAU RIVER NR HOT SPRING ID
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1910–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at BRUNEAU RIVER NR HOT SPRING IDLargest measured flow of each year at BRUNEAU RIVER NR HOT SPRING ID: BRUNEAU RIVER NR HOT SPRING ID in m³/s, from 1910 to 2025.Hurricane Katrina water and sanitation collapse050100150200m³/s19101953196319741984199420052016

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
PeriodBRUNEAU RIVER NR HOT SPRING ID (m³/s)
1910184
194456.9
194582.4
194656.1
194734.8
194845.6
194987.8
195065.4
195151.5
1952104
195360.9
195426.1
195528.6
195672.8
1957116
195860.3
195926.2
196044.5
196121.1
196291.2
1963170
196445.9
196619.9
1967126
196849.0
196966.3
197077.3
1971130
197275.9
197352.7
197455.8
1975141
197660.9
197737.9
197842.8
197972.8
198055.5
198123.1
198269.1
198399.7
1984194
198557.2
1986107
198725.5
198827.5
198957.2
199026.3
199134.8
199211.8
199388.9
199434.0
199594.6
199667.1
1997113
199875.3
199961.7
200128.6
200236.2
200345.9
200447.3
2005159
200696.6
200854.9
200945.0
201071.9
2011138
201226.6
2013137
201426.0
201545.9
201681.6
2017164
201841.1
2019117
202045.6
202115.8
202232.6
202377.6
202462.0
202533.1

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 held1910–2025
Completeness69.0% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 4 separate periods inside 1910–2025 hold no value. The longest runs from 1911 to 1943 — 33 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1910 and is not continuous from it: 116 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 BRUNEAU RIVER NR HOT SPRING ID, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1910–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above BRUNEAU RIVER NR HOT SPRING ID, as a depthWater leaving the catchment above BRUNEAU RIVER NR HOT SPRING ID, as a depth: BRUNEAU RIVER NR HOT SPRING ID in mm, from 1910 to 2025.Hurricane Katrina water and sanitation collapse050100150mm19101950196119721983199420052016

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
PeriodBRUNEAU RIVER NR HOT SPRING ID (mm)
191069.0
191151.0
191273.0
191350.0
191466.0
194449.0
194567.0
194647.0
194734.0
194839.0
194956.0
195059.0
195155.0
195275.0
195345.0
195423.0
195526.0
195649.0
195762.0
195847.0
195923.0
196036.0
196120.0
196259.0
196351.0
196452.0
196561.0
196620.0
196737.0
196827.0
196955.0
197060.0
1971102
197275.0
197345.0
197449.0
197586.0
197652.0
197725.0
197847.0
197950.0
198056.0
198120.0
198266.0
198372.0
1984131
198548.0
198667.0
198721.0
198828.0
198949.0
199026.0
199129.0
199214.0
199354.0
199423.0
199564.0
199655.0
199765.0
199862.0
199948.0
200025.0
200120.0
200230.0
200326.0
200432.0
200557.0
200666.0
200724.0
200835.0
200944.0
201043.0
201191.0
201222.0
201323.0
201420.0
201525.0
201665.0
201790.0
201828.0
201971.0
202038.0
202118.0
202229.0
202353.0
202449.0
202533.0

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 held1910–2025
Completeness75.0% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • One period inside 1910–2025 holds no value: 1915 to 1943, 29 years with no reading. It is drawn as a break in the line and is never interpolated across.
ContinuityThe record begins in 1910 and is not continuous from it: 116 years separate the first value from the last, and 75% 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

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

636
Fullest snowpack recorded at Seventysix Creek, in 1984 (mm of water)
78
Thinnest, in 1992 (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 Seventysix Creek
Water years 1979–2026. Each point is the fullest month of that snow season.
Peak snowpack at Seventysix CreekPeak snowpack at Seventysix Creek: Seventysix Creek in mm, from 1979 to 2026.0200400600800mm19791985199119972003200920152021Seventysix Creek 1979: 382 mmSeventysix Creek 1980: 274 mmSeventysix Creek 1981: 82.0 mmSeventysix Creek 1982: 457 mmSeventysix Creek 1983: 428 mmSeventysix Creek 1984: 636 mmSeventysix Creek 1985: 272 mmSeventysix Creek 1986: 339 mmSeventysix Creek 1987: 114 mmSeventysix Creek 1988: 135 mmSeventysix Creek 1989: 316 mmSeventysix Creek 1990: 211 mmSeventysix Creek 1991: 156 mmSeventysix Creek 1992: 78.0 mmSeventysix Creek 1993: 373 mmSeventysix Creek 1994: 165 mmSeventysix Creek 1995: 273 mmSeventysix Creek 1996: 328 mmSeventysix Creek 1997: 383 mmSeventysix Creek 1998: 318 mmSeventysix Creek 1999: 278 mmSeventysix Creek 2000: 306 mmSeventysix Creek 2001: 166 mmSeventysix Creek 2002: 313 mmSeventysix Creek 2003: 158 mmSeventysix Creek 2004: 292 mmSeventysix Creek 2005: 226 mmSeventysix Creek 2006: 428 mmSeventysix Creek 2007: 157 mmSeventysix Creek 2008: 280 mmSeventysix Creek 2009: 201 mmSeventysix Creek 2010: 205 mmSeventysix Creek 2011: 259 mmSeventysix Creek 2012: 209 mmSeventysix Creek 2013: 159 mmSeventysix Creek 2014: 152 mmSeventysix Creek 2015: 167 mmSeventysix Creek 2016: 234 mmSeventysix Creek 2017: 387 mmSeventysix Creek 2018: 112 mmSeventysix Creek 2019: 392 mmSeventysix Creek 2020: 259 mmSeventysix Creek 2021: 190 mmSeventysix Creek 2022: 137 mmSeventysix Creek 2023: 368 mmSeventysix Creek 2024: 351 mmSeventysix Creek 2025: 323 mmSeventysix Creek 2026: 85.0 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
PeriodSeventysix Creek (mm)
1979382
1980274
198182.0
1982457
1983428
1984636
1985272
1986339
1987114
1988135
1989316
1990211
1991156
199278.0
1993373
1994165
1995273
1996328
1997383
1998318
1999278
2000306
2001166
2002313
2003158
2004292
2005226
2006428
2007157
2008280
2009201
2010205
2011259
2012209
2013159
2014152
2015167
2016234
2017387
2018112
2019392
2020259
2021190
2022137
2023368
2024351
2025323
202685.0

Read against the river

Seventysix Creek and BRUNEAU RIVER NR HOT SPRING ID both sit in this drainage area, and their records overlap by 46 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 Bruneau and what each holds
GaugeMeasuresValuesRecord
BRUNEAU RIVER NR HOT SPRING IDburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2921909–2026
BRUNEAU RV AT ROWLAND, NVburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2281913–2026
EF BRUNEAU RIVER NR HOT SPRING IDcatchment area, annual maximum river flow261911–2026

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 — 17050102. 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
BRUNEAU RIVER NR HOT SPRING IDStated 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
BRUNEAU RV AT ROWLAND, NVStated 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
EF BRUNEAU RIVER NR HOT SPRING IDStated 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 4 of them, which makes it a full profile.

Information-gain signals held for this water body
SignalHeldCounts
Gauges holding a real record2no
Years spanned118yes, 20 or more
Values held2,236yes, 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), Bruneau gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-bruneau/

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 Bruneau 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 confidence2025-05-12

Source: USGS — National Water Information System, USGS site 13168500, 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.