The monitoring network within this area

Hydrionis holds 2,800 values from 4 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.

4
Gauges
2,800
Values held
1895–2026
Record spans
Gauges within the Upper Humboldt huc8 subbasin
4 monitoring points, positioned as the publisher records them.
Gauges within the Upper Humboldt huc8 subbasinLAMOILLE CK NR LAMOILLE, NV, HUMBOLDT RV NR ELKO, NV, HUMBOLDT RV AT PALISADE, NV, MAGGIE CK AT CARLIN, NVLAMOILLE CK NR LAMOILLE, NVHUMBOLDT RV NR ELKO, NVHUMBOLDT RV AT PALISADE, NVMAGGIE CK AT CARLIN, NV

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 LAMOILLE CK NR LAMOILLE, NV
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 LAMOILLE CK NR LAMOILLE, NVLargest measured flow of each year at LAMOILLE CK NR LAMOILLE, NV: LAMOILLE CK NR LAMOILLE, NV in m³/s, from 1915 to 2025.Hurricane Katrina water and sanitation collapse010203040m³/s19151948196019721984199620082020

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
PeriodLAMOILLE CK NR LAMOILLE, NV (m³/s)
19158.92
19169.34
19188.50
191910.2
192010.7
192111.3
192211.8
19239.97
19449.66
194513.8
19468.47
19479.23
194810.8
19499.34
195016.7
195114.3
195211.8
19538.81
19546.65
19559.15
195612.7
195722.5
195812.9
19596.74
19609.85
19619.63
196211.8
196316.1
196413.4
196512.7
19666.97
196713.4
196811.1
196910.4
197019.3
197120.2
197217.5
197318.7
197411.3
197515.9
19768.24
197710.2
197811.3
197915.2
198013.5
19817.14
198223.5
198320.8
198419.1
198512.6
198623.7
19878.41
19888.86
19899.68
199010.2
199113.4
19924.53
199314.6
19948.75
199522.3
199620.8
199723.7
199815.7
199918.2
200013.4
200116.5
200213.5
200322.4
20047.96
200521.5
200621.7
20076.46
200813.6
200911.2
201032.3
201121.0
20125.75
20136.43
201410.1
201520.8
201620.0
201719.7
20189.20
201918.2
20207.62
202118.5
202210.7
202321.2
202412.9
202513.9

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
Completeness81.1% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 2 separate periods inside 1915–2025 hold no value. The longest runs from 1924 to 1943 — 20 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 81% 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 HUMBOLDT RV AT PALISADE, 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. 1903–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above HUMBOLDT RV AT PALISADE, NV, as a depthWater leaving the catchment above HUMBOLDT RV AT PALISADE, NV, as a depth: HUMBOLDT RV AT PALISADE, NV in mm, from 1903 to 2025.Hurricane Katrina water and sanitation collapse050100mm19031924193919541969198419992014

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
PeriodHUMBOLDT RV AT PALISADE, NV (mm)
190323.0
190437.0
190519.0
191231.0
191323.0
191451.0
19158.00
191623.0
191744.0
19188.00
191916.0
192013.0
192159.0
192242.0
192323.0
19249.00
192532.0
19267.00
192724.0
192813.0
192911.0
193010.0
19313.00
193230.0
193312.0
19342.00
193515.0
193626.0
193718.0
193822.0
193916.0
194014.0
194127.0
194252.0
194355.0
194427.0
194557.0
194637.0
194715.0
194813.0
194922.0
195026.0
195129.0
195260.0
195316.0
19546.00
19556.00
195633.0
195730.0
195829.0
19595.00
19608.00
19617.00
196236.0
196324.0
196430.0
196535.0
196611.0
196723.0
196813.0
196942.0
197030.0
197158.0
197227.0
197336.0
197425.0
197556.0
197618.0
19778.00
197823.0
197932.0
198047.0
19817.00
198247.0
198388.0
1984124
198526.0
198650.0
198710.0
198810.0
198925.0
199011.0
199110.0
19926.00
199332.0
199410.0
199544.0
199640.0
199748.0
199851.0
199929.0
200016.0
20018.00
200213.0
200312.0
200414.0
200557.0
200667.0
200712.0
200814.0
200920.0
201020.0
201152.0
20129.00
20135.00
20148.00
20158.00
201631.0
201772.0
201814.0
201955.0
202012.0
20215.00
20225.00
202347.0
202435.0
202515.0

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 held1903–2025
Completeness95.1% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • One period inside 1903–2025 holds no value: 1906 to 1911, 6 years with no reading. It is drawn as a break in the line and is never interpolated across.
ContinuityThe record begins in 1903 and is not continuous from it: 123 years separate the first value from the last, and 95% 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

4 automated snow stations sit inside this drainage area, weighing the snowpack rather than measuring how deep it is.

921
Fullest snowpack recorded at Dorsey Basin, in 1984 (mm of water)
102
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 Dorsey Basin
Water years 1979–2026. Each point is the fullest month of that snow season.
Peak snowpack at Dorsey BasinPeak snowpack at Dorsey Basin: Dorsey Basin in mm, from 1979 to 2026.02505007501,000mm19791985199119972003200920152021Dorsey Basin 1979: 533 mmDorsey Basin 1980: 408 mmDorsey Basin 1981: 200 mmDorsey Basin 1982: 553 mmDorsey Basin 1983: 728 mmDorsey Basin 1984: 921 mmDorsey Basin 1985: 338 mmDorsey Basin 1986: 304 mmDorsey Basin 1987: 243 mmDorsey Basin 1988: 299 mmDorsey Basin 1989: 476 mmDorsey Basin 1990: 366 mmDorsey Basin 1991: 281 mmDorsey Basin 1992: 188 mmDorsey Basin 1993: 391 mmDorsey Basin 1994: 223 mmDorsey Basin 1995: 325 mmDorsey Basin 1996: 398 mmDorsey Basin 1997: 340 mmDorsey Basin 1998: 455 mmDorsey Basin 1999: 362 mmDorsey Basin 2000: 389 mmDorsey Basin 2001: 243 mmDorsey Basin 2002: 299 mmDorsey Basin 2003: 275 mmDorsey Basin 2004: 298 mmDorsey Basin 2005: 471 mmDorsey Basin 2006: 597 mmDorsey Basin 2007: 215 mmDorsey Basin 2008: 371 mmDorsey Basin 2009: 356 mmDorsey Basin 2010: 372 mmDorsey Basin 2011: 475 mmDorsey Basin 2012: 217 mmDorsey Basin 2013: 281 mmDorsey Basin 2014: 302 mmDorsey Basin 2015: 195 mmDorsey Basin 2016: 314 mmDorsey Basin 2017: 451 mmDorsey Basin 2018: 231 mmDorsey Basin 2019: 508 mmDorsey Basin 2020: 290 mmDorsey Basin 2021: 288 mmDorsey Basin 2022: 192 mmDorsey Basin 2023: 630 mmDorsey Basin 2024: 504 mmDorsey Basin 2025: 387 mmDorsey Basin 2026: 102 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
PeriodDorsey Basin (mm)
1979533
1980408
1981200
1982553
1983728
1984921
1985338
1986304
1987243
1988299
1989476
1990366
1991281
1992188
1993391
1994223
1995325
1996398
1997340
1998455
1999362
2000389
2001243
2002299
2003275
2004298
2005471
2006597
2007215
2008371
2009356
2010372
2011475
2012217
2013281
2014302
2015195
2016314
2017451
2018231
2019508
2020290
2021288
2022192
2023630
2024504
2025387
2026102

Read against the river

Dorsey Basin and LAMOILLE CK NR LAMOILLE, NV both sit in this drainage area, and their records overlap by 46 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 Humboldt and what each holds
GaugeMeasuresValuesRecord
HUMBOLDT RV AT PALISADE, NVburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3621902–2026
LAMOILLE CK NR LAMOILLE, NVburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3051915–2026
HUMBOLDT RV NR ELKO, NVburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2931895–2026
MAGGIE CK AT CARLIN, NVcatchment area, annual maximum river flow401914–2026

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 — 16040101. 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
HUMBOLDT RV AT PALISADE, 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
LAMOILLE CK NR LAMOILLE, 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
HUMBOLDT RV NR ELKO, 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
MAGGIE CK AT CARLIN, 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

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 spanned132yes, 20 or more
Values held2,800yes, 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 Humboldt gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-upper-humboldt/

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 Humboldt 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 confidence2025-06-01

Source: USGS — National Water Information System, USGS site 10322500, 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.