The monitoring network within this area

Hydrionis holds 1,681 values from 5 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.

5
Gauges
1,681
Values held
1911–2026
Record spans
Gauges within the Upper Salmon huc8 subbasin
5 monitoring points, positioned as the publisher records them.
Gauges within the Upper Salmon huc8 subbasinVALLEY CREEK AT STANLEY ID, SALMON RIVER BL YANKEE FORK NR CLAYTON ID, YANKEE FORK SALMON RIVER NR CLAYTON ID, BIG BOULDER CREEK NR CLAYTON ID, EF SALMON RIVER NR CLAYTON IDVALLEY CREEK AT STANLEY IDSALMON RIVER BL YANKEE FORK NR CLAYTON IDYANKEE FORK SALMON RIVER NR CLAYTON IDBIG BOULDER CREEK NR CLAYTON IDEF SALMON RIVER NR CLAYTON 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 SALMON RIVER BL YANKEE FORK NR CLAYTON ID
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1923–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at SALMON RIVER BL YANKEE FORK NR CLAYTON IDLargest measured flow of each year at SALMON RIVER BL YANKEE FORK NR CLAYTON ID: SALMON RIVER BL YANKEE FORK NR CLAYTON ID in m³/s, from 1923 to 2025.Hurricane Katrina water and sanitation collapse0100200300m³/s19231938194919601971198320032015

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
PeriodSALMON RIVER BL YANKEE FORK NR CLAYTON ID (m³/s)
1923139
192666.8
1927227
1928213
192997.4
1930106
1932152
1933181
193483.3
1936183
193774.2
1938192
193974.2
1940107
194195.4
1942158
1943204
194480.1
194592.0
1946125
1947172
1948200
1949139
1950163
1951202
1952169
1953162
1954185
1955144
1956292
1957217
1958203
1959135
1960114
1961110
1962112
1963135
1964132
1965233
196686.6
1967176
1968106
1969165
1970180
1971212
1972247
197393.7
1974297
1975170
1976146
197738.8
1978150
1980136
1981175
1982225
1983202
1984171
1985112
1986242
198766.3
198883.0
1989106
199075.0
199192.6
200168.0
2002129
2003204
200472.8
2005102
2006229
200793.2
2009164
2010228
2011168
2012200
2013106
2014145
201575.3
2016114
2017249
2018154
2019135
2020112
202167.4
2022198
2023177
2024115
2025128

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 held1923–2025
Completeness85.4% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 6 separate periods inside 1923–2025 hold no value. The longest runs from 1992 to 2000 — 9 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1923 and is not continuous from it: 103 years separate the first value from the last, and 85% 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 SALMON RIVER BL YANKEE FORK NR CLAYTON 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. 1922–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above SALMON RIVER BL YANKEE FORK NR CLAYTON ID, as a depthWater leaving the catchment above SALMON RIVER BL YANKEE FORK NR CLAYTON ID, as a depth: SALMON RIVER BL YANKEE FORK NR CLAYTON ID in mm, from 1922 to 2025.Hurricane Katrina water and sanitation collapse02505007501,000mm19221933194419551966198320042015

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
PeriodSALMON RIVER BL YANKEE FORK NR CLAYTON ID (mm)
1922470
1923415
1924245
1925499
1926251
1927527
1928479
1929288
1930344
1931231
1932404
1933375
1934309
1935335
1936415
1937254
1938497
1939276
1940358
1941340
1942407
1943685
1944343
1945337
1946461
1947479
1948469
1949412
1950531
1951601
1952498
1953467
1954502
1955389
1956678
1957504
1958492
1959421
1960352
1961313
1962411
1963454
1964417
1965681
1966310
1967478
1968365
1969491
1970491
1977196
1978466
1979291
1980439
1981379
1982631
1983564
1984509
1985376
1986548
1987242
1988277
1989336
1990302
2001211
2002328
2003378
2004305
2005291
2006496
2007340
2008426
2009446
2010392
2011518
2012514
2013335
2014458
2015336
2016432
2017816
2018496
2019435
2020344
2021261
2022415
2023435
2024349
2025403

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 held1922–2025
Completeness84.6% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 2 separate periods inside 1922–2025 hold no value. The longest runs from 1991 to 2000 — 10 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1922 and is not continuous from it: 104 years separate the first value from the last, and 85% 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.

1,469
Fullest snowpack recorded at Vienna Mine, in 1982 (mm of water)
451
Thinnest, in 1987 (mm of water)
April
Month the pack is usually at its fullest
July
Month the pack has gone by, in half of years
Peak snowpack at Vienna Mine
Water years 1982–2026. Each point is the fullest month of that snow season.
Peak snowpack at Vienna MinePeak snowpack at Vienna Mine: Vienna Mine in mm, from 1982 to 2026.05001,0001,500mm19821989199520012007201320192025Vienna Mine 1982: 1,469 mmVienna Mine 1983: 1,248 mmVienna Mine 1985: 730 mmVienna Mine 1986: 1,166 mmVienna Mine 1987: 451 mmVienna Mine 1988: 650 mmVienna Mine 1989: 873 mmVienna Mine 1990: 574 mmVienna Mine 1991: 669 mmVienna Mine 1992: 542 mmVienna Mine 1993: 992 mmVienna Mine 1994: 484 mmVienna Mine 1995: 1,259 mmVienna Mine 1996: 1,176 mmVienna Mine 1997: 1,396 mmVienna Mine 1998: 815 mmVienna Mine 1999: 1,037 mmVienna Mine 2000: 784 mmVienna Mine 2001: 458 mmVienna Mine 2002: 802 mmVienna Mine 2003: 982 mmVienna Mine 2004: 680 mmVienna Mine 2005: 559 mmVienna Mine 2006: 1,194 mmVienna Mine 2007: 595 mmVienna Mine 2008: 903 mmVienna Mine 2009: 805 mmVienna Mine 2010: 622 mmVienna Mine 2011: 983 mmVienna Mine 2012: 931 mmVienna Mine 2013: 688 mmVienna Mine 2014: 880 mmVienna Mine 2015: 641 mmVienna Mine 2016: 882 mmVienna Mine 2017: 1,412 mmVienna Mine 2018: 834 mmVienna Mine 2019: 906 mmVienna Mine 2020: 652 mmVienna Mine 2021: 603 mmVienna Mine 2022: 750 mmVienna Mine 2023: 932 mmVienna Mine 2024: 718 mmVienna Mine 2025: 810 mmVienna Mine 2026: 806 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
PeriodVienna Mine (mm)
19821,469
19831,248
1985730
19861,166
1987451
1988650
1989873
1990574
1991669
1992542
1993992
1994484
19951,259
19961,176
19971,396
1998815
19991,037
2000784
2001458
2002802
2003982
2004680
2005559
20061,194
2007595
2008903
2009805
2010622
2011983
2012931
2013688
2014880
2015641
2016882
20171,412
2018834
2019906
2020652
2021603
2022750
2023932
2024718
2025810
2026806

Read against the river

Vienna Mine and VALLEY CREEK AT STANLEY 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 Upper Salmon and what each holds
GaugeMeasuresValuesRecord
SALMON RIVER BL YANKEE FORK NR CLAYTON IDburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3041921–2026
VALLEY CREEK AT STANLEY IDburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2681911–2026
YANKEE FORK SALMON RIVER NR CLAYTON IDcatchment area, annual maximum river flow341922–2026
EF SALMON RIVER NR CLAYTON IDcatchment area, annual maximum river flow111929–2026
BIG BOULDER CREEK NR CLAYTON IDcatchment area, annual maximum river flow51926–2026

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 — 17060201. 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
SALMON RIVER BL YANKEE FORK NR CLAYTON 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
VALLEY CREEK AT STANLEY 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
YANKEE FORK SALMON RIVER NR CLAYTON 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
EF SALMON RIVER NR CLAYTON 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
BIG BOULDER CREEK NR CLAYTON 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 spanned116yes, 20 or more
Values held1,681yes, 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), Upper Salmon gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-upper-salmon/

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 Upper Salmon 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 13296500, 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.