The monitoring network within this area

Hydrionis holds 903 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
903
Values held
1910–2026
Record spans
Gauges within the Salmon Falls huc8 subbasin
2 monitoring points, positioned as the publisher records them.
Gauges within the Salmon Falls huc8 subbasinSALMON FALLS CREEK NR SAN JACINTO NV, CEDAR CREEK NR ROSEWORTH IDSALMON FALLS CREEK NR SAN JACINTO NVCEDAR CREEK NR ROSEWORTH 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 FALLS CREEK NR SAN JACINTO NV
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1911–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at SALMON FALLS CREEK NR SAN JACINTO NVLargest measured flow of each year at SALMON FALLS CREEK NR SAN JACINTO NV: SALMON FALLS CREEK NR SAN JACINTO NV in m³/s, from 1911 to 2025.Hurricane Katrina water and sanitation collapse050100m³/s19111926193919521965197819932014

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 FALLS CREEK NR SAN JACINTO NV (m³/s)
191130.0
191236.8
191318.8
191423.7
19156.97
191617.7
191923.4
192016.5
192133.1
192233.1
192314.8
192418.3
192520.7
19269.91
192723.2
192816.8
192914.8
193010.6
19315.78
193221.9
193313.5
19342.78
193516.5
193622.5
193710.3
193822.7
193949.8
19409.57
19418.95
194238.8
194357.8
194425.2
194526.9
194625.4
19479.68
194815.5
194928.3
195022.6
195134.5
195240.5
195313.6
19545.66
195510.5
195624.3
195734.8
195824.7
19598.64
196017.8
19616.68
196255.8
196320.4
196424.0
196523.4
19669.49
196718.2
19689.17
196926.1
197031.7
197138.8
197232.0
197324.0
197440.5
197568.8
197628.3
19777.62
197818.8
197924.6
198040.5
19817.82
198229.2
198335.7
1984109
198640.8
198812.5
198923.8
19908.21
19919.74
19923.37
199330.3
199410.00
199546.7
199624.4
199726.8
200540.5
200713.8
200818.4
200928.2
201019.2
201143.9
201218.5
20139.43
201410.9
201514.8
201623.2
2017114
20189.51
201944.5
202018.1
20215.32
202210.7
202332.0
202422.8
202513.3

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 held1911–2025
Completeness89.6% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 5 separate periods inside 1911–2025 hold no value. The longest runs from 1998 to 2004 — 7 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1911 and is not continuous from it: 115 years separate the first value from the last, and 90% 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 FALLS CREEK NR SAN JACINTO NV, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1911–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above SALMON FALLS CREEK NR SAN JACINTO NV, as a depthWater leaving the catchment above SALMON FALLS CREEK NR SAN JACINTO NV, as a depth: SALMON FALLS CREEK NR SAN JACINTO NV in mm, from 1911 to 2025.Hurricane Katrina water and sanitation collapse0255075100mm19111930194419581972198620002014

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 FALLS CREEK NR SAN JACINTO NV (mm)
191134.0
191254.0
191336.0
191445.0
191517.0
192029.0
192241.0
192334.0
192426.0
192536.0
192618.0
192733.0
192829.0
192929.0
193018.0
193113.0
193237.0
193324.0
193411.0
193526.0
193631.0
193720.0
193836.0
193928.0
194019.0
194121.0
194252.0
194358.0
194440.0
194545.0
194635.0
194721.0
194831.0
194939.0
195040.0
195147.0
195252.0
195327.0
195415.0
195519.0
195638.0
195743.0
195836.0
195918.0
196027.0
196114.0
196251.0
196331.0
196442.0
196547.0
196617.0
196730.0
196819.0
196941.0
197044.0
197167.0
197256.0
197342.0
197442.0
197561.0
197642.0
197718.0
197839.0
197941.0
198050.0
198115.0
198247.0
198355.0
1984109
198541.0
198651.0
198717.0
198825.0
198937.0
199020.0
199122.0
199212.0
199345.0
199417.0
199549.0
199645.0
199754.0
199845.0
199938.0
200022.0
200115.0
200226.0
200318.0
200426.0
200539.0
200656.0
200722.0
200825.0
200942.0
201031.0
201165.0
201219.0
201319.0
201420.0
201523.0
201645.0
201773.0
201819.0
201955.0
202030.0
202114.0
202222.0
202347.0
202435.0
202522.0

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 held1911–2025
Completeness95.7% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 2 separate periods inside 1911–2025 hold no value. The longest runs from 1916 to 1919 — 4 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1911 and is not continuous from it: 115 years separate the first value from the last, and 96% 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.

563
Fullest snowpack recorded at Wilson Creek, in 2023 (mm of water)
72
Thinnest, in 2026 (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 Wilson Creek
Water years 1991–2026. Each point is the fullest month of that snow season.
Peak snowpack at Wilson CreekPeak snowpack at Wilson Creek: Wilson Creek in mm, from 1991 to 2026.0200400600mm19911996200120062011201620212026Wilson Creek 1991: 254 mmWilson Creek 1992: 188 mmWilson Creek 1993: 349 mmWilson Creek 1994: 223 mmWilson Creek 1995: 268 mmWilson Creek 1996: 362 mmWilson Creek 1997: 420 mmWilson Creek 1998: 336 mmWilson Creek 1999: 340 mmWilson Creek 2000: 377 mmWilson Creek 2001: 261 mmWilson Creek 2002: 371 mmWilson Creek 2003: 190 mmWilson Creek 2004: 392 mmWilson Creek 2005: 205 mmWilson Creek 2006: 501 mmWilson Creek 2007: 228 mmWilson Creek 2008: 406 mmWilson Creek 2009: 410 mmWilson Creek 2010: 353 mmWilson Creek 2011: 456 mmWilson Creek 2012: 186 mmWilson Creek 2013: 328 mmWilson Creek 2014: 244 mmWilson Creek 2015: 240 mmWilson Creek 2016: 380 mmWilson Creek 2017: 303 mmWilson Creek 2018: 177 mmWilson Creek 2019: 379 mmWilson Creek 2020: 334 mmWilson Creek 2021: 308 mmWilson Creek 2022: 239 mmWilson Creek 2023: 563 mmWilson Creek 2024: 387 mmWilson Creek 2025: 324 mmWilson Creek 2026: 72.0 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
PeriodWilson Creek (mm)
1991254
1992188
1993349
1994223
1995268
1996362
1997420
1998336
1999340
2000377
2001261
2002371
2003190
2004392
2005205
2006501
2007228
2008406
2009410
2010353
2011456
2012186
2013328
2014244
2015240
2016380
2017303
2018177
2019379
2020334
2021308
2022239
2023563
2024387
2025324
202672.0

Read against the river

Wilson Creek and SALMON FALLS CREEK NR SAN JACINTO NV both sit in this drainage area, and their records overlap by 34 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 Salmon Falls and what each holds
GaugeMeasuresValuesRecord
SALMON FALLS CREEK NR SAN JACINTO NVburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3601910–2026
CEDAR CREEK NR ROSEWORTH IDcatchment area, annual maximum river flow121910–2026

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 — 17040213. 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 FALLS CREEK NR SAN JACINTO 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
CEDAR CREEK NR ROSEWORTH 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 spanned117yes, 20 or more
Values held903no
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), Salmon Falls gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-salmon-falls/

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 Salmon Falls 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 confidence2025-02-25

Source: USGS — National Water Information System, USGS site 13105000, 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.