The monitoring network within this area

Hydrionis holds 464 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
464
Values held
1890–2026
Record spans
Gauges within the Upper Missouri-Dearborn huc8 subbasin
2 monitoring points, positioned as the publisher records them.
Gauges within the Upper Missouri-Dearborn huc8 subbasinMissouri River at Fort Benton MT, Missouri River at Cascade MTMissouri River at Fort Benton MTMissouri River at Cascade 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 Missouri River at Fort Benton MT
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1891–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at Missouri River at Fort Benton MTLargest measured flow of each year at Missouri River at Fort Benton MT: Missouri River at Fort Benton MT in m³/s, from 1891 to 2025.Hurricane Katrina water and sanitation collapse01,0002,0003,0004,000m³/s18911908192519431959197819952011

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
PeriodMissouri River at Fort Benton MT (m³/s)
18911,124
18921,863
18931,008
18941,566
1895606
18961,144
1897773
18981,065
18991,303
1901861
1902900
1903861
1904773
1905450
1906561
19071,345
19083,964
19091,540
1910665
1911903
19131,246
1914818
1915869
19161,376
19171,365
1918793
1919394
1920869
1921912
1922971
1923719
1924688
1925844
1926578
1928946
1929609
1931368
1932665
1933742
1934555
1935487
1936680
1937300
1938866
1939507
1940385
1941433
1942940
19431,090
1944878
1945677
1946535
1947968
19481,495
1949643
1950818
1951779
1952694
19532,229
1954507
1955450
1956881
1957606
1958580
1959779
1960583
1961292
1962651
1963629
19642,192
1965881
19671,093
1968807
1969833
1970799
1971753
1972694
1974827
19751,756
1976940
1978665
1979583
1980796
19811,447
1982827
1983665
1984739
1986606
1987337
1988237
1989450
1990430
1991682
1992232
1993668
1994436
1995801
1996855
19971,039
1998821
1999555
2000223
2001188
2002450
2003402
2004258
2005484
2006564
2007405
2008903
2009580
2010850
20111,492
2012459
2013436
2014487
2015354
2016379
2017481
20181,141
2019801
2020566
2021382
2022323
2023680
2024354
2025255

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 held1891–2025
Completeness94.1% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 8 separate periods inside 1891–2025 hold no value. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1891 and is not continuous from it: 135 years separate the first value from the last, and 94% 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 Missouri River at Fort Benton 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. 1891–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above Missouri River at Fort Benton MT, as a depthWater leaving the catchment above Missouri River at Fort Benton MT, as a depth: Missouri River at Fort Benton MT in mm, from 1891 to 2025.Hurricane Katrina water and sanitation collapse050100150200mm18911908192519421959197619932010

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
PeriodMissouri River at Fort Benton MT (mm)
1891122
1892142
1893129
1894168
1895100
1896129
1897114
1898137
1899155
1900105
190195.0
190293.0
1903105
1904117
190568.0
190685.0
1907154
1908170
1909144
1910114
1911107
1912134
1913151
1914121
1915129
1916159
1917160
1918109
191963.0
1920115
1921111
1922118
1923110
192490.0
1925119
192697.0
1927161
1928135
192996.0
193074.0
193155.0
193279.0
193386.0
193465.0
193563.0
193666.0
193749.0
193890.0
193974.0
194062.0
194165.0
1942111
1943135
194496.0
194585.0
194689.0
1947126
1948149
194993.0
1950108
1951120
1952115
1953107
195475.0
195584.0
195699.0
195794.0
195894.0
1959106
196090.0
196167.0
196292.0
196397.0
1964134
1965164
196686.0
1967131
1968127
1969137
1970138
1971138
1972130
197381.0
1974120
1975181
1976154
197778.0
1978138
1979104
1980117
1981134
1982143
1983122
1984139
198591.0
1986107
198768.0
198862.0
198984.0
199079.0
199199.0
199262.0
1993131
199485.0
1995129
1996131
1997153
1998120
1999105
200072.0
200162.0
200269.0
200376.0
200466.0
200581.0
200687.0
200774.0
2008103
2009104
2010117
2011178
201291.0
201374.0
2014102
201580.0
201677.0
201794.0
2018138
2019115
2020101
202171.0
202270.0
2023107
202479.0
202570.0

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 held1891–2025
Completeness100.0% of the periods in that span are held.
ContinuityContinuous: every year from 1891 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

Every gauge Hydrionis holds within this area

Gauges within the Upper Missouri-Dearborn and what each holds
GaugeMeasuresValuesRecord
Missouri River at Fort Benton MTburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year4381890–2026
Missouri River at Cascade MTcatchment area, annual maximum river flow261903–2026

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 — 10030102. 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
Missouri River at Fort Benton 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
Missouri River at Cascade 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 3 of them, which makes it a full profile.

Information-gain signals held for this water body
SignalHeldCounts
Gauges holding a real record1no
Years spanned137yes, 20 or more
Values held464no
Distinct measurements5yes, 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 Missouri-Dearborn gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-upper-missouri-dearborn/

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 Missouri-Dearborn 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 confidence2025-05-20

Source: USGS — National Water Information System, USGS site 06090800, 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.