The monitoring network within this area

Hydrionis holds 1,220 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
1,220
Values held
1906–2026
Record spans
Gauges within the Payette huc8 subbasin
3 monitoring points, positioned as the publisher records them.
Gauges within the Payette huc8 subbasinPAYETTE RIVER NR HORSESHOE BEND ID, PAYETTE RIVER NR EMMETT ID, PAYETTE RIVER NR BANKS IDPAYETTE RIVER NR HORSESHOE BEND IDPAYETTE RIVER NR EMMETT IDPAYETTE RIVER NR BANKS 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 PAYETTE RIVER NR HORSESHOE BEND ID
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1915–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at PAYETTE RIVER NR HORSESHOE BEND IDLargest measured flow of each year at PAYETTE RIVER NR HORSESHOE BEND ID: PAYETTE RIVER NR HORSESHOE BEND ID in m³/s, from 1915 to 2025.Hurricane Katrina water and sanitation collapse0200400600800m³/s19151933194819621976198920022016

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
PeriodPAYETTE RIVER NR HORSESHOE BEND ID (m³/s)
1915266
1916555
1920328
1921626
1923405
1924247
1925462
1926281
1927595
1929314
1930243
1931186
1932476
1933535
1934250
1935289
1936535
1937241
1938569
1940382
1942408
1943566
1944209
1945323
1946442
1947479
1948433
1949385
1950345
1951379
1952470
1953473
1954362
1955227
1957436
1958422
1959251
1960286
1961209
1962222
1963377
1964337
1966169
1967311
1968155
1969340
1970433
1971578
1972405
1973178
1974547
1975362
1976331
197779.9
1978328
1979184
1980297
1981396
1982425
1983510
1984408
1985255
1986456
1987130
1988122
1989247
1990174
1991127
1992109
1993357
1994126
1995340
1996459
1997691
1998377
1999377
2000242
2001134
2002331
2003413
2004230
2005279
2006459
2007179
2008399
2009351
2010609
2011396
2012521
2014326
2015191
2016280
2017467
2018317
2019464
2020292
2021137
2022362
2023399
2024309
2025317

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 held1915–2025
Completeness91.0% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 8 separate periods inside 1915–2025 hold no value. The longest runs from 1917 to 1919 — 3 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1915 and is not continuous from it: 111 years separate the first value from the last, and 91% 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 PAYETTE RIVER NR HORSESHOE BEND 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. 1907–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above PAYETTE RIVER NR HORSESHOE BEND ID, as a depthWater leaving the catchment above PAYETTE RIVER NR HORSESHOE BEND ID, as a depth: PAYETTE RIVER NR HORSESHOE BEND ID in mm, from 1907 to 2025.Hurricane Katrina water and sanitation collapse2004006008001,000mm19071926194119561971198620012016

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
PeriodPAYETTE RIVER NR HORSESHOE BEND ID (mm)
1907789
1908473
1909695
1910638
1911600
1912546
1913545
1914477
1915326
1920423
1921686
1922493
1923458
1924233
1925532
1926294
1927712
1928559
1929310
1930331
1931218
1932504
1933422
1934344
1935346
1936457
1937312
1938613
1939331
1940487
1941440
1942461
1943752
1944295
1945430
1946603
1947533
1948512
1949490
1950571
1951603
1952631
1953555
1954555
1955409
1956677
1957604
1958555
1959461
1960486
1961393
1962434
1963537
1964494
1965733
1966423
1967443
1968388
1969583
1970568
1971779
1972650
1973379
1974822
1975536
1976540
1977232
1978547
1979361
1980538
1981485
1982785
1983730
1984651
1985422
1986624
1987265
1988265
1989402
1990319
1991284
1992265
1993514
1994267
1995605
1996770
1997829
1998553
1999632
2000431
2001241
2002366
2003467
2004384
2005348
2006627
2007359
2008485
2009446
2010426
2011599
2012569
2013347
2014453
2015324
2016449
2017804
2018462
2019533
2020391
2021304
2022385
2023441
2024406
2025488

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 held1907–2025
Completeness96.6% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • One period inside 1907–2025 holds no value: 1916 to 1919, 4 years with no reading. It is drawn as a break in the line and is never interpolated across.
ContinuityThe record begins in 1907 and is not continuous from it: 119 years separate the first value from the last, and 97% 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

1 automated snow station sits inside this drainage area, weighing the snowpack rather than measuring how deep it is.

955
Fullest snowpack recorded at Bogus Basin, in 2023 (mm of water)
248
Thinnest, in 2026 (mm of water)
March
Month the pack is usually at its fullest
June
Month the pack has gone by, in half of years
Peak snowpack at Bogus Basin
Water years 2000–2026. Each point is the fullest month of that snow season.
Peak snowpack at Bogus BasinPeak snowpack at Bogus Basin: Bogus Basin in mm, from 2000 to 2026.02505007501,000mm2000200420082012201620202024Bogus Basin 2000: 709 mmBogus Basin 2001: 464 mmBogus Basin 2002: 644 mmBogus Basin 2003: 528 mmBogus Basin 2004: 708 mmBogus Basin 2005: 477 mmBogus Basin 2006: 803 mmBogus Basin 2007: 520 mmBogus Basin 2008: 743 mmBogus Basin 2009: 608 mmBogus Basin 2010: 576 mmBogus Basin 2011: 765 mmBogus Basin 2012: 485 mmBogus Basin 2013: 347 mmBogus Basin 2014: 578 mmBogus Basin 2015: 324 mmBogus Basin 2016: 626 mmBogus Basin 2017: 643 mmBogus Basin 2018: 385 mmBogus Basin 2019: 765 mmBogus Basin 2020: 550 mmBogus Basin 2021: 626 mmBogus Basin 2022: 404 mmBogus Basin 2023: 955 mmBogus Basin 2024: 675 mmBogus Basin 2025: 757 mmBogus Basin 2026: 248 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
PeriodBogus Basin (mm)
2000709
2001464
2002644
2003528
2004708
2005477
2006803
2007520
2008743
2009608
2010576
2011765
2012485
2013347
2014578
2015324
2016626
2017643
2018385
2019765
2020550
2021626
2022404
2023955
2024675
2025757
2026248

Read against the river

Bogus Basin and PAYETTE RIVER NR HORSESHOE BEND ID both sit in this drainage area, and their records overlap by 25 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 Payette and what each holds
GaugeMeasuresValuesRecord
PAYETTE RIVER NR HORSESHOE BEND IDburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3711906–2026
PAYETTE RIVER NR EMMETT IDburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3371925–2026
PAYETTE RIVER NR BANKS IDburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year1881921–2026

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 — 17050122. 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
PAYETTE RIVER NR HORSESHOE BEND 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
PAYETTE RIVER NR EMMETT 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
PAYETTE RIVER NR BANKS 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 5 of them, which makes it a full profile.

Information-gain signals held for this water body
SignalHeldCounts
Gauges holding a real record3yes, 3 or more
Years spanned121yes, 20 or more
Values held1,220yes, 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), Payette gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-payette/

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 Payette 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 13247500, 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.