The monitoring network within this area

Hydrionis holds 1,712 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
1,712
Values held
1898–2026
Record spans
Gauges within the Portneuf huc8 subbasin
3 monitoring points, positioned as the publisher records them.
Gauges within the Portneuf huc8 subbasinPORTNEUF RIVER AT TOPAZ ID, PORTNEUF RIVER AT POCATELLO ID, PORTNEUF RIVER NR PEBBLE IDPORTNEUF RIVER AT TOPAZ IDPORTNEUF RIVER AT POCATELLO IDPORTNEUF RIVER NR PEBBLE 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 PORTNEUF RIVER AT POCATELLO ID
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1919–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at PORTNEUF RIVER AT POCATELLO IDLargest measured flow of each year at PORTNEUF RIVER AT POCATELLO ID: PORTNEUF RIVER AT POCATELLO ID in m³/s, from 1919 to 2025.Hurricane Katrina water and sanitation collapse0255075100m³/s19191945195619681980199220092020

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
PeriodPORTNEUF RIVER AT POCATELLO ID (m³/s)
191923.6
192916.7
193113.3
193217.5
193314.6
19348.50
193820.2
194013.0
194116.5
194220.6
194325.3
194521.9
194629.4
194715.7
194820.8
194919.4
195025.5
195117.8
195229.7
195317.6
195414.4
195510.6
195618.7
195727.5
195821.6
195914.5
196021.5
196118.3
196284.7
196371.1
196421.9
196620.1
196718.1
196817.0
196932.0
197024.4
197144.7
197235.7
197327.8
197436.5
197543.6
197639.4
197823.2
197916.0
198033.7
198235.7
198356.4
198481.3
198537.1
198641.3
198721.8
198814.8
198924.9
199014.3
199115.5
199215.1
199330.6
199420.7
199517.4
199636.2
199736.8
200015.8
200212.5
200413.6
200723.7
200812.9
200919.6
201014.2
201134.3
201222.9
201313.6
201419.0
20159.15
201617.5
201731.4
201827.9
201927.8
202017.6
202110.1
202210.0
202337.1
202428.9
202517.3

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 held1919–2025
Completeness77.6% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 12 separate periods inside 1919–2025 hold no value. The longest runs from 1920 to 1928 — 9 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1919 and is not continuous from it: 107 years separate the first value from the last, and 78% 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 PORTNEUF RIVER AT POCATELLO 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. 1913–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above PORTNEUF RIVER AT POCATELLO ID, as a depthWater leaving the catchment above PORTNEUF RIVER AT POCATELLO ID, as a depth: PORTNEUF RIVER AT POCATELLO ID in mm, from 1913 to 2025.Hurricane Katrina water and sanitation collapse050100150200mm19131928194219561970198419982012

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
PeriodPORTNEUF RIVER AT POCATELLO ID (mm)
191375.0
1914109
191559.0
191675.0
191876.0
191969.0
192078.0
1921115
1922100
192388.0
192460.0
192580.0
192658.0
192781.0
192869.0
192970.0
193049.0
193141.0
193262.0
193355.0
193429.0
193543.0
193664.0
193756.0
193869.0
193953.0
194044.0
194157.0
194266.0
194385.0
194465.0
194592.0
194695.0
194762.0
194877.0
194969.0
1950110
195174.0
195286.0
195370.0
195450.0
195547.0
195659.0
195773.0
195871.0
195954.0
196048.0
196144.0
196270.0
196365.0
196475.0
196592.0
196650.0
196769.0
196863.0
196993.0
197077.0
1971129
1972134
197395.0
1974110
1975126
1976110
197748.0
197881.0
197957.0
1980101
198162.0
1982117
1983171
1984194
1985107
1986167
198767.0
198847.0
198959.0
199044.0
199150.0
199229.0
199375.0
199440.0
199564.0
199694.0
1997125
1998110
199994.0
200058.0
200137.0
200242.0
200330.0
200436.0
200556.0
200696.0
200748.0
200844.0
200965.0
201051.0
201199.0
201252.0
201337.0
201440.0
201536.0
201651.0
2017109
201874.0
201985.0
202063.0
202139.0
202240.0
202394.0
202486.0
202558.0

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 held1913–2025
Completeness99.1% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • One period inside 1913–2025 holds no value: 1917. 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: 113 years separate the first value from the last, and 99% 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.

687
Fullest snowpack recorded at Wildhorse Divide, in 1982 (mm of water)
162
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 Wildhorse Divide
Water years 1982–2026. Each point is the fullest month of that snow season.
Peak snowpack at Wildhorse DividePeak snowpack at Wildhorse Divide: Wildhorse Divide in mm, from 1982 to 2026.0200400600800mm1982199119972003200920152021Wildhorse Divide 1982: 687 mmWildhorse Divide 1986: 450 mmWildhorse Divide 1987: 241 mmWildhorse Divide 1988: 257 mmWildhorse Divide 1989: 506 mmWildhorse Divide 1990: 282 mmWildhorse Divide 1991: 352 mmWildhorse Divide 1992: 169 mmWildhorse Divide 1993: 488 mmWildhorse Divide 1994: 280 mmWildhorse Divide 1995: 372 mmWildhorse Divide 1996: 526 mmWildhorse Divide 1997: 606 mmWildhorse Divide 1998: 546 mmWildhorse Divide 1999: 466 mmWildhorse Divide 2000: 410 mmWildhorse Divide 2001: 294 mmWildhorse Divide 2002: 435 mmWildhorse Divide 2003: 269 mmWildhorse Divide 2004: 515 mmWildhorse Divide 2005: 308 mmWildhorse Divide 2006: 606 mmWildhorse Divide 2007: 292 mmWildhorse Divide 2008: 433 mmWildhorse Divide 2009: 459 mmWildhorse Divide 2010: 285 mmWildhorse Divide 2011: 515 mmWildhorse Divide 2012: 251 mmWildhorse Divide 2013: 254 mmWildhorse Divide 2014: 272 mmWildhorse Divide 2015: 237 mmWildhorse Divide 2016: 354 mmWildhorse Divide 2017: 448 mmWildhorse Divide 2018: 267 mmWildhorse Divide 2019: 476 mmWildhorse Divide 2020: 337 mmWildhorse Divide 2021: 292 mmWildhorse Divide 2022: 261 mmWildhorse Divide 2023: 653 mmWildhorse Divide 2024: 548 mmWildhorse Divide 2025: 521 mmWildhorse Divide 2026: 162 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
PeriodWildhorse Divide (mm)
1982687
1986450
1987241
1988257
1989506
1990282
1991352
1992169
1993488
1994280
1995372
1996526
1997606
1998546
1999466
2000410
2001294
2002435
2003269
2004515
2005308
2006606
2007292
2008433
2009459
2010285
2011515
2012251
2013254
2014272
2015237
2016354
2017448
2018267
2019476
2020337
2021292
2022261
2023653
2024548
2025521
2026162

Read against the river

Wildhorse Divide and PORTNEUF RIVER AT TOPAZ ID both sit in this drainage area, and their records overlap by 43 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 Portneuf and what each holds
GaugeMeasuresValuesRecord
PORTNEUF RIVER AT POCATELLO IDburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3471898–2026
PORTNEUF RIVER AT TOPAZ IDburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3211913–2026
PORTNEUF RIVER NR PEBBLE IDcatchment area, annual maximum river flow101969–2026

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 — 17040208. 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
PORTNEUF RIVER AT POCATELLO 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
PORTNEUF RIVER AT TOPAZ 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
PORTNEUF RIVER NR PEBBLE 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 spanned129yes, 20 or more
Values held1,712yes, 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), Portneuf gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-portneuf/

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 Portneuf 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 confidence2025-04-13

Source: USGS — National Water Information System, USGS site 13075500, 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.