The monitoring network within this area

Hydrionis holds 1,719 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
1,719
Values held
1909–2026
Record spans
Gauges within the Lake Walcott huc8 subbasin
5 monitoring points, positioned as the publisher records them.
Gauges within the Lake Walcott huc8 subbasinSNAKE RIVER AT NEELEY ID, SOUTH SIDE MINIDOKA CANAL NR MINIDOKA ID, SNAKE R NR MINIDOKA ID AT HOWELLS FERRY, P A LATERAL NR MILNER ID, SOUTH SIDE TWIN FALLS CANAL AT MILNER IDSNAKE RIVER AT NEELEY IDSOUTH SIDE MINIDOKA CANAL NR MINIDOKA IDSNAKE R NR MINIDOKA ID AT HOWELLS FERRYP A LATERAL NR MILNER IDSOUTH SIDE TWIN FALLS CANAL AT MILNER 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 SNAKE R NR MINIDOKA ID AT HOWELLS FERRY
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1914–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at SNAKE R NR MINIDOKA ID AT HOWELLS FERRYLargest measured flow of each year at SNAKE R NR MINIDOKA ID AT HOWELLS FERRY: SNAKE R NR MINIDOKA ID AT HOWELLS FERRY in m³/s, from 1914 to 2025.Hurricane Katrina water and sanitation collapse05001,0001,500m³/s19141928194519571969198220012017

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
PeriodSNAKE R NR MINIDOKA ID AT HOWELLS FERRY (m³/s)
19141,031
1916685
1917988
19181,300
1919402
1920629
1921932
1922801
1923612
1925705
1926255
1927909
1928748
1929425
1931230
1932251
1934208
1937385
1939377
1940251
1941241
1942572
1943847
1944674
1945665
1946716
1947765
1948702
1949405
1950759
1951603
1952600
1953609
1954510
1955297
1956767
1957705
1958357
1959300
1960292
1961261
1962510
1963719
1964807
1965538
1966280
1967515
1968532
1969589
1970606
1971801
1972620
1973402
1974612
1975547
1976702
1978368
1979518
1980708
1981603
1982648
1983739
1984748
1985572
1986733
1988286
1989306
1990292
1993549
1996580
19971,215
2000328
2001262
2006614
2007303
2008362
2009665
2010309
2011787
2012382
2013309
2014374
2015326
2016365
2017697
2018583
2019595
2020408
2021385
2022278
2023365
2024538
2025379

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 held1914–2025
Completeness83.0% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 12 separate periods inside 1914–2025 hold no value. The longest runs from 2002 to 2005 — 4 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1914 and is not continuous from it: 112 years separate the first value from the last, and 83% 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 SNAKE R NR MINIDOKA ID AT HOWELLS FERRY, 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 SNAKE R NR MINIDOKA ID AT HOWELLS FERRY, as a depthWater leaving the catchment above SNAKE R NR MINIDOKA ID AT HOWELLS FERRY, as a depth: SNAKE R NR MINIDOKA ID AT HOWELLS FERRY in mm, from 1911 to 2025.Hurricane Katrina water and sanitation collapse100200300mm19111926194119561971198620012016

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
PeriodSNAKE R NR MINIDOKA ID AT HOWELLS FERRY (mm)
1911204
1912239
1913237
1914203
1915122
1916193
1917227
1918203
1919108
1920144
1921185
1922158
1923155
192488.0
1925176
192697.0
1927151
1928183
1929130
1930103
193186.0
193290.0
193393.0
193470.0
193575.0
1936101
193793.0
1938121
1939116
194087.0
194186.0
1942108
1943180
1944118
1945135
1946159
1947138
1948149
1949139
1950175
1951192
1952182
1953129
1954124
1955108
1956169
1957141
1958117
195998.0
196097.0
196174.0
1962120
1963119
1964144
1965187
1966127
1967118
1968124
1969154
1970153
1971268
1972237
1973148
1974209
1975208
1976227
197793.0
1978123
1979137
1980134
1981126
1982207
1983257
1984273
1985176
1986261
1987108
198883.0
198994.0
199092.0
199190.0
199279.0
1993102
1994109
1995122
1996200
1997313
1998207
1999209
2000130
200184.0
200281.0
200381.0
200474.0
200577.0
2006124
200796.0
200893.0
2009138
2010101
2011232
2012126
201388.0
201495.0
2015101
201687.0
2017194
2018190
2019135
2020127
202194.0
202278.0
202390.0
2024116
202596.0

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
Completeness100.0% of the periods in that span are held.
ContinuityContinuous: every year from 1911 to 2025 is held.
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.

1,170
Fullest snowpack recorded at Howell Canyon, in 2006 (mm of water)
197
Thinnest, in 1981 (mm of water)
April
Month the pack is usually at its fullest
June
Month the pack has gone by, in half of years
Peak snowpack at Howell Canyon
Water years 1981–2026. Each point is the fullest month of that snow season.
Peak snowpack at Howell CanyonPeak snowpack at Howell Canyon: Howell Canyon in mm, from 1981 to 2026.05001,000mm19811987199319992005201120172023Howell Canyon 1981: 197 mmHowell Canyon 1982: 993 mmHowell Canyon 1983: 840 mmHowell Canyon 1984: 953 mmHowell Canyon 1985: 472 mmHowell Canyon 1986: 932 mmHowell Canyon 1987: 311 mmHowell Canyon 1988: 436 mmHowell Canyon 1989: 639 mmHowell Canyon 1990: 302 mmHowell Canyon 1991: 411 mmHowell Canyon 1992: 319 mmHowell Canyon 1993: 864 mmHowell Canyon 1994: 327 mmHowell Canyon 1995: 537 mmHowell Canyon 1996: 741 mmHowell Canyon 1997: 1,116 mmHowell Canyon 1998: 796 mmHowell Canyon 1999: 708 mmHowell Canyon 2000: 633 mmHowell Canyon 2001: 317 mmHowell Canyon 2002: 656 mmHowell Canyon 2003: 351 mmHowell Canyon 2004: 649 mmHowell Canyon 2005: 557 mmHowell Canyon 2006: 1,170 mmHowell Canyon 2007: 636 mmHowell Canyon 2008: 791 mmHowell Canyon 2009: 690 mmHowell Canyon 2010: 562 mmHowell Canyon 2011: 938 mmHowell Canyon 2012: 577 mmHowell Canyon 2013: 599 mmHowell Canyon 2014: 704 mmHowell Canyon 2015: 659 mmHowell Canyon 2016: 807 mmHowell Canyon 2017: 945 mmHowell Canyon 2018: 570 mmHowell Canyon 2019: 715 mmHowell Canyon 2020: 591 mmHowell Canyon 2021: 612 mmHowell Canyon 2022: 642 mmHowell Canyon 2023: 864 mmHowell Canyon 2024: 824 mmHowell Canyon 2025: 674 mmHowell Canyon 2026: 435 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
PeriodHowell Canyon (mm)
1981197
1982993
1983840
1984953
1985472
1986932
1987311
1988436
1989639
1990302
1991411
1992319
1993864
1994327
1995537
1996741
19971,116
1998796
1999708
2000633
2001317
2002656
2003351
2004649
2005557
20061,170
2007636
2008791
2009690
2010562
2011938
2012577
2013599
2014704
2015659
2016807
2017945
2018570
2019715
2020591
2021612
2022642
2023864
2024824
2025674
2026435

Read against the river

Howell Canyon and SNAKE RIVER AT NEELEY ID both sit in this drainage area, and their records overlap by 44 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 Lake Walcott and what each holds
GaugeMeasuresValuesRecord
SNAKE R NR MINIDOKA ID AT HOWELLS FERRYburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3651910–2026
SNAKE RIVER AT NEELEY IDburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3241914–2026
SOUTH SIDE MINIDOKA CANAL NR MINIDOKA IDburned area within 50 km, mean river flow, mean river flow, water year1661909–2019
SOUTH SIDE TWIN FALLS CANAL AT MILNER IDburned area within 50 km, mean river flow, mean river flow, water year1651909–2019
P A LATERAL NR MILNER IDburned area within 50 km, mean river flow, mean river flow, water year1471919–2019

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 — 17040209. 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
SNAKE R NR MINIDOKA ID AT HOWELLS FERRYStated 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
SNAKE RIVER AT NEELEY 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
SOUTH SIDE MINIDOKA CANAL NR MINIDOKA 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
SOUTH SIDE TWIN FALLS CANAL AT MILNER 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
P A LATERAL NR MILNER 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 5 of them, which makes it a full profile.

Information-gain signals held for this water body
SignalHeldCounts
Gauges holding a real record5yes, 3 or more
Years spanned118yes, 20 or more
Values held1,719yes, 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), Lake Walcott gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-lake-walcott/

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 Lake Walcott 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 confidence2025-06-23

Source: USGS — National Water Information System, USGS site 13081500, 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.