The monitoring network within this area

Hydrionis holds 1,427 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
1,427
Values held
1910–2026
Record spans
Gauges within the Lower Clark Fork huc8 subbasin
3 monitoring points, positioned as the publisher records them.
Gauges within the Lower Clark Fork huc8 subbasinCLARK FORK AT WHITEHORSE RAPIDS NR CABINET ID, Clark Fork near Plains MT, Thompson River near Thompson Falls MTCLARK FORK AT WHITEHORSE RAPIDS NR CABINET IDClark Fork near Plains MTThompson River near Thompson Falls MT

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 Clark Fork near Plains MT
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1912–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at Clark Fork near Plains MTLargest measured flow of each year at Clark Fork near Plains MT: Clark Fork near Plains MT in m³/s, from 1912 to 2025.Hurricane Katrina water and sanitation collapse01,0002,0003,0004,000m³/s19121927194219571972198720022017

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
PeriodClark Fork near Plains MT (m³/s)
19122,110
19133,256
19141,897
19151,073
19163,256
19173,002
19182,832
19192,090
19202,090
19212,832
19223,228
19232,733
19242,274
19253,002
19261,354
19273,313
19283,568
19291,906
19301,339
19311,339
19322,367
19333,398
19342,175
19352,016
19362,316
19371,416
19382,492
19391,926
19401,362
1941912
19422,095
19432,619
19441,025
19452,121
19462,008
19472,945
19483,794
19492,721
19503,115
19512,721
19522,047
19532,653
19542,566
19552,118
19563,002
19572,461
19582,696
19592,628
19602,155
19612,650
19621,914
19631,657
19643,625
19652,577
19661,665
19672,704
19681,971
19691,943
19702,532
19712,537
19723,256
1973895
19743,200
19753,030
19762,481
1977597
19781,889
19792,070
19802,413
19812,687
19822,563
19831,974
19841,736
19851,574
19862,175
19871,014
1988827
19891,665
19901,866
19912,098
1992852
19931,430
1994895
19952,087
19962,557
19973,115
19981,668
19991,784
20001,206
2001830
20022,441
20031,880
20041,155
20051,977
20062,115
20071,419
20082,149
20091,645
20101,657
20112,945
20122,132
20131,804
20142,345
20151,036
20161,249
20172,325
20182,917
20191,928
20202,240
20211,662
20222,407
20231,583
20241,158
20251,017

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 held1912–2025
Completeness100.0% of the periods in that span are held.
ContinuityContinuous: every year from 1912 to 2025 is held.
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 Clark Fork near Plains MT, 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 Clark Fork near Plains MT, as a depthWater leaving the catchment above Clark Fork near Plains MT, as a depth: Clark Fork near Plains MT in mm, from 1911 to 2025.Hurricane Katrina water and sanitation collapse200400600mm19111926194119561971198620012016

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
PeriodClark Fork near Plains MT (mm)
1911333
1912330
1913416
1914310
1915263
1916485
1917418
1918411
1919247
1920323
1921381
1922333
1923339
1924276
1925423
1926240
1927485
1928467
1929248
1930248
1931189
1932338
1933426
1934399
1935288
1936277
1937213
1938298
1939273
1940196
1941175
1942289
1943427
1944179
1945252
1946340
1947424
1948430
1949323
1950448
1951451
1952322
1953303
1954396
1955340
1956454
1957333
1958303
1959490
1960348
1961347
1962350
1963301
1964402
1965461
1966318
1967380
1968336
1969398
1970342
1971436
1972465
1973224
1974483
1975407
1976425
1977200
1978364
1979316
1980322
1981379
1982385
1983318
1984307
1985311
1986328
1987231
1988222
1989316
1990369
1991393
1992224
1993292
1994222
1995311
1996485
1997507
1998295
1999334
2000270
2001170
2002337
2003258
2004258
2005278
2006336
2007277
2008345
2009292
2010276
2011492
2012399
2013291
2014393
2015273
2016285
2017396
2018429
2019282
2020344
2021277
2022345
2023237
2024227
2025230

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.

2,301
Fullest snowpack recorded at Bear Mountain, in 1997 (mm of water)
614
Thinnest, in 2015 (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 Bear Mountain
Water years 1984–2026. Each point is the fullest month of that snow season.
Peak snowpack at Bear MountainPeak snowpack at Bear Mountain: Bear Mountain in mm, from 1984 to 2026.01,0002,000mm1984199119982004201020162022Bear Mountain 1984: 1,043 mmBear Mountain 1985: 1,566 mmBear Mountain 1986: 933 mmBear Mountain 1987: 1,355 mmBear Mountain 1988: 1,290 mmBear Mountain 1990: 1,449 mmBear Mountain 1991: 1,848 mmBear Mountain 1992: 1,038 mmBear Mountain 1993: 1,158 mmBear Mountain 1995: 1,564 mmBear Mountain 1996: 1,317 mmBear Mountain 1997: 2,301 mmBear Mountain 1998: 1,211 mmBear Mountain 1999: 2,268 mmBear Mountain 2000: 1,599 mmBear Mountain 2001: 725 mmBear Mountain 2002: 1,998 mmBear Mountain 2003: 1,471 mmBear Mountain 2004: 1,322 mmBear Mountain 2005: 1,017 mmBear Mountain 2006: 1,729 mmBear Mountain 2007: 1,416 mmBear Mountain 2008: 1,653 mmBear Mountain 2009: 1,258 mmBear Mountain 2010: 1,083 mmBear Mountain 2011: 1,899 mmBear Mountain 2012: 1,895 mmBear Mountain 2013: 1,433 mmBear Mountain 2014: 1,475 mmBear Mountain 2015: 614 mmBear Mountain 2016: 1,159 mmBear Mountain 2017: 1,270 mmBear Mountain 2018: 1,615 mmBear Mountain 2019: 1,039 mmBear Mountain 2020: 1,620 mmBear Mountain 2021: 1,163 mmBear Mountain 2022: 1,287 mmBear Mountain 2023: 1,015 mmBear Mountain 2024: 1,119 mmBear Mountain 2025: 1,456 mmBear Mountain 2026: 874 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
PeriodBear Mountain (mm)
19841,043
19851,566
1986933
19871,355
19881,290
19901,449
19911,848
19921,038
19931,158
19951,564
19961,317
19972,301
19981,211
19992,268
20001,599
2001725
20021,998
20031,471
20041,322
20051,017
20061,729
20071,416
20081,653
20091,258
20101,083
20111,899
20121,895
20131,433
20141,475
2015614
20161,159
20171,270
20181,615
20191,039
20201,620
20211,163
20221,287
20231,015
20241,119
20251,456
2026874

Read against the river

Bear Mountain and CLARK FORK AT WHITEHORSE RAPIDS NR CABINET ID both sit in this drainage area, and their records overlap by 29 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 Lower Clark Fork and what each holds
GaugeMeasuresValuesRecord
Clark Fork near Plains MTburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3811910–2026
CLARK FORK AT WHITEHORSE RAPIDS NR CABINET IDburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2631928–2026
Thompson River near Thompson Falls MTburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2461948–2026

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 — 17010213. 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
Clark Fork near Plains MTStated 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
CLARK FORK AT WHITEHORSE RAPIDS NR CABINET 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
Thompson River near Thompson Falls MTStated 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 spanned117yes, 20 or more
Values held1,427yes, 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), Lower Clark Fork gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-lower-clark-fork/

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 Lower Clark Fork 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 confidence2025-05-13

Source: USGS — National Water Information System, USGS site 12389000, 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.