The monitoring network within this area

Hydrionis holds 674 values from 2 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.

2
Gauges
674
Values held
1908–2026
Record spans
Gauges within the North Fork Payette huc8 subbasin
2 monitoring points, positioned as the publisher records them.
Gauges within the North Fork Payette huc8 subbasinNF PAYETTE RIVER AT MCCALL ID, GOLD FORK RIVER NR ROSEBERRY IDNF PAYETTE RIVER AT MCCALL IDGOLD FORK RIVER NR ROSEBERRY 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 NF PAYETTE RIVER AT MCCALL ID
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1924–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at NF PAYETTE RIVER AT MCCALL IDLargest measured flow of each year at NF PAYETTE RIVER AT MCCALL ID: NF PAYETTE RIVER AT MCCALL ID in m³/s, from 1924 to 2025.Hurricane Katrina water and sanitation collapse050100150m³/s19241939195219651978199120042017

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
PeriodNF PAYETTE RIVER AT MCCALL ID (m³/s)
192470.5
192585.5
192653.8
192798.0
192968.8
193049.3
193147.0
193294.0
193456.6
193565.1
193693.4
193756.6
193897.4
193959.5
194070.8
194170.8
194297.4
194397.4
194487.2
194568.5
194669.1
194798.3
1948121
194991.5
195082.1
195168.0
195288.6
195375.3
195491.2
195579.9
1956101
195787.8
1958100
195970.5
196077.6
196191.2
196266.0
196376.7
196491.7
196592.3
196666.3
1967105
196865.7
196982.1
1970108
1971104
1972108
197370.8
1974140
197594.3
197666.3
197721.2
197880.4
197966.3
198069.4
1981109
1982100
1983108
1984100
198569.1
1986114
198729.7
198877.0
198968.2
199054.9
199153.2
199239.6
199390.9
199439.6
199591.2
1996129
1997122
199892.6
1999121
200066.5
200172.2
200288.1
2003136
200471.6
200586.9
2006141
200763.1
2008101
200993.4
2010139
201196.8
201284.4
201388.6
201483.5
201534.0
201690.6
2017111
201879.3
201984.1
2020111
202159.2
202279.6
2023101
2024118
202587.8

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 held1924–2025
Completeness98.0% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 2 separate periods inside 1924–2025 hold no value. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1924 and is not continuous from it: 102 years separate the first value from the last, and 98% 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 NF PAYETTE RIVER AT MCCALL 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. 1909–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above NF PAYETTE RIVER AT MCCALL ID, as a depthWater leaving the catchment above NF PAYETTE RIVER AT MCCALL ID, as a depth: NF PAYETTE RIVER AT MCCALL ID in mm, from 1909 to 2025.Hurricane Katrina water and sanitation collapse5001,0001,500mm19091927194219571972198720022017

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
PeriodNF PAYETTE RIVER AT MCCALL ID (mm)
19091,165
1910958
19111,094
1912850
19131,005
1914860
1915551
19161,093
1920743
19211,136
1922831
1923810
1924434
1925947
1926615
19271,224
1928888
1929569
1930657
1931384
1932903
1933778
1934670
1935686
1936742
1937551
19381,166
1939613
1940849
1941875
1942805
19431,130
1944495
1945830
1946897
1947990
19481,093
1949820
19501,049
1951959
19521,093
1953897
1954940
1955735
19561,115
1957912
1958922
1959937
1960784
1961788
1962976
1963855
1964874
19651,216
1966618
19671,036
1968794
1969912
19701,091
19711,254
1972986
1973719
19741,453
19751,023
1976871
1977330
19781,092
1979575
1980957
1981840
19821,268
19831,120
19841,021
1985662
1986950
1987361
1988483
1989732
1990615
1991562
1992431
1993913
1994411
19951,252
19961,310
19971,357
1998962
19991,112
2000760
2001413
2002765
2003912
2004773
2005658
20061,132
2007681
2008907
2009805
2010778
20111,097
20121,012
2013717
2014838
2015560
2016896
20171,294
2018719
2019888
2020702
2021488
2022700
2023686
2024636
2025863

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 held1909–2025
Completeness97.4% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • One period inside 1909–2025 holds no value: 1917 to 1919, 3 years with no reading. It is drawn as a break in the line and is never interpolated across.
ContinuityThe record begins in 1909 and is not continuous from it: 117 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.

406
Fullest snowpack recorded at Long Valley, in 2019 (mm of water)
47
Thinnest, in 2026 (mm of water)
March
Month the pack is usually at its fullest
April
Month the pack has gone by, in half of years
Peak snowpack at Long Valley
Water years 2002–2026. Each point is the fullest month of that snow season.
Peak snowpack at Long ValleyPeak snowpack at Long Valley: Long Valley in mm, from 2002 to 2026.0200400mm2002200620102014201820222026Long Valley 2002: 261 mmLong Valley 2003: 93.0 mmLong Valley 2004: 204 mmLong Valley 2005: 83.0 mmLong Valley 2006: 250 mmLong Valley 2007: 128 mmLong Valley 2008: 340 mmLong Valley 2009: 99.0 mmLong Valley 2010: 178 mmLong Valley 2011: 178 mmLong Valley 2012: 120 mmLong Valley 2013: 81.0 mmLong Valley 2014: 96.0 mmLong Valley 2015: 65.0 mmLong Valley 2016: 215 mmLong Valley 2017: 200 mmLong Valley 2018: 98.0 mmLong Valley 2019: 406 mmLong Valley 2020: 249 mmLong Valley 2021: 239 mmLong Valley 2022: 173 mmLong Valley 2023: 210 mmLong Valley 2024: 144 mmLong Valley 2025: 215 mmLong Valley 2026: 47.0 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
PeriodLong Valley (mm)
2002261
200393.0
2004204
200583.0
2006250
2007128
2008340
200999.0
2010178
2011178
2012120
201381.0
201496.0
201565.0
2016215
2017200
201898.0
2019406
2020249
2021239
2022173
2023210
2024144
2025215
202647.0

Read against the river

Long Valley and NF PAYETTE RIVER AT MCCALL ID both sit in this drainage area, and their records overlap by 23 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 North Fork Payette and what each holds
GaugeMeasuresValuesRecord
NF PAYETTE RIVER AT MCCALL IDburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3651908–2026
GOLD FORK RIVER NR ROSEBERRY IDcatchment area, annual maximum river flow91962–2026

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 — 17050123. 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
NF PAYETTE RIVER AT MCCALL 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
GOLD FORK RIVER NR ROSEBERRY 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 3 of them, which makes it a full profile.

Information-gain signals held for this water body
SignalHeldCounts
Gauges holding a real record1no
Years spanned119yes, 20 or more
Values held674no
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), North Fork Payette gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-north-fork-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 North Fork 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 confidence2025-05-31

Source: USGS — National Water Information System, USGS site 13239000, 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.