The monitoring network within this area

Hydrionis holds 767 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
767
Values held
1851–2026
Record spans
Gauges within the Lower Des Moines huc8 subbasin
4 monitoring points, positioned as the publisher records them.
Gauges within the Lower Des Moines huc8 subbasinDes Moines River near Tracy, IA, Des Moines River at Ottumwa, IA, Des Moines River at Keosauqua, IA, Sugar Creek near Keokuk, IADes Moines River near Tracy, IADes Moines River at Ottumwa, IADes Moines River at Keosauqua, IASugar Creek near Keokuk, IA

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 Des Moines River at Keosauqua, IA
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1851–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at Des Moines River at Keosauqua, IALargest measured flow of each year at Des Moines River at Keosauqua, IA: Des Moines River at Keosauqua, IA in m³/s, from 1851 to 2025.Hurricane Katrina water and sanitation collapse02,0004,000m³/s18511922193819541970198520012017

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
PeriodDes Moines River at Keosauqua, IA (m³/s)
18510
19034,134
19041,252
19053,058
1906954
19121,600
1913753
1914903
19151,914
19161,314
19171,931
19181,195
19191,286
19201,249
1921767
1922782
1923742
19241,144
1925589
19261,070
19271,237
1928561
19291,184
1930833
1931552
1933954
1934280
19351,540
1936762
19371,433
1938711
19391,328
1940442
1941742
19431,000
19442,047
19451,402
19462,217
19473,511
19481,495
1949898
19501,079
19511,798
19521,215
1953895
19541,722
1956328
1957603
1958957
19591,172
19602,090
19611,022
19621,455
1963665
1964765
19652,260
1966915
19671,405
1968524
19691,127
1970705
19711,000
1972694
19732,044
19741,090
1975722
19761,923
1977532
19781,150
19791,090
19801,167
19811,269
19821,923
19831,008
19841,320
1985770
19861,809
1987354
1989445
19901,373
19911,348
19921,039
19933,143
1994626
19951,385
19961,586
1997966
19981,464
19991,172
20001,399
20011,461
20021,005
2003643
20041,011
2005782
2006555
20072,073
20083,002
20091,195
20102,554
20111,979
2012637
20132,339
20141,359
20151,628
20171,308
2018991
20192,588
20201,062
20211,699
2022623
2023756
20241,354
2025934

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 held1851–2025
Completeness65.1% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 7 separate periods inside 1851–2025 hold no value. The longest runs from 1852 to 1902 — 51 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1851 and is not continuous from it: 175 years separate the first value from the last, and 65% 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 Des Moines River at Keosauqua, IA, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1970–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above Des Moines River at Keosauqua, IA, as a depthWater leaving the catchment above Des Moines River at Keosauqua, IA, as a depth: Des Moines River at Keosauqua, IA in mm, from 1970 to 2025.Hurricane Katrina water and sanitation collapse0200400600800mm19701977198419911998200520122019Des Moines River at Keosauqua, IA 1970: 114 mmDes Moines River at Keosauqua, IA 1971: 129 mmDes Moines River at Keosauqua, IA 1972: 166 mmDes Moines River at Keosauqua, IA 1973: 446 mmDes Moines River at Keosauqua, IA 1974: 226 mmDes Moines River at Keosauqua, IA 1975: 152 mmDes Moines River at Keosauqua, IA 1976: 102 mmDes Moines River at Keosauqua, IA 1977: 61.0 mmDes Moines River at Keosauqua, IA 1978: 163 mmDes Moines River at Keosauqua, IA 1979: 265 mmDes Moines River at Keosauqua, IA 1980: 100 mmDes Moines River at Keosauqua, IA 1981: 86.0 mmDes Moines River at Keosauqua, IA 1982: 312 mmDes Moines River at Keosauqua, IA 1983: 373 mmDes Moines River at Keosauqua, IA 1984: 343 mmDes Moines River at Keosauqua, IA 1985: 123 mmDes Moines River at Keosauqua, IA 1986: 331 mmDes Moines River at Keosauqua, IA 1987: 177 mmDes Moines River at Keosauqua, IA 1988: 52.0 mmDes Moines River at Keosauqua, IA 1989: 33.0 mmDes Moines River at Keosauqua, IA 1990: 202 mmDes Moines River at Keosauqua, IA 1991: 304 mmDes Moines River at Keosauqua, IA 1992: 268 mmDes Moines River at Keosauqua, IA 1993: 631 mmDes Moines River at Keosauqua, IA 1994: 148 mmDes Moines River at Keosauqua, IA 1995: 232 mmDes Moines River at Keosauqua, IA 1996: 212 mmDes Moines River at Keosauqua, IA 1997: 191 mmDes Moines River at Keosauqua, IA 1998: 294 mmDes Moines River at Keosauqua, IA 1999: 243 mmDes Moines River at Keosauqua, IA 2000: 63.0 mmDes Moines River at Keosauqua, IA 2001: 244 mmDes Moines River at Keosauqua, IA 2002: 106 mmDes Moines River at Keosauqua, IA 2003: 136 mmDes Moines River at Keosauqua, IA 2004: 195 mmDes Moines River at Keosauqua, IA 2005: 159 mmDes Moines River at Keosauqua, IA 2006: 121 mmDes Moines River at Keosauqua, IA 2007: 367 mmDes Moines River at Keosauqua, IA 2008: 420 mmDes Moines River at Keosauqua, IA 2009: 297 mmDes Moines River at Keosauqua, IA 2010: 600 mmDes Moines River at Keosauqua, IA 2011: 290 mmDes Moines River at Keosauqua, IA 2012: 63.0 mmDes Moines River at Keosauqua, IA 2013: 195 mmDes Moines River at Keosauqua, IA 2014: 247 mmDes Moines River at Keosauqua, IA 2015: 356 mmDes Moines River at Keosauqua, IA 2016: 363 mmDes Moines River at Keosauqua, IA 2017: 229 mmDes Moines River at Keosauqua, IA 2018: 432 mmDes Moines River at Keosauqua, IA 2019: 467 mmDes Moines River at Keosauqua, IA 2020: 196 mmDes Moines River at Keosauqua, IA 2021: 95.0 mmDes Moines River at Keosauqua, IA 2022: 105 mmDes Moines River at Keosauqua, IA 2023: 85.0 mmDes Moines River at Keosauqua, IA 2024: 210 mmDes Moines River at Keosauqua, IA 2025: 202 mm

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
PeriodDes Moines River at Keosauqua, IA (mm)
1970114
1971129
1972166
1973446
1974226
1975152
1976102
197761.0
1978163
1979265
1980100
198186.0
1982312
1983373
1984343
1985123
1986331
1987177
198852.0
198933.0
1990202
1991304
1992268
1993631
1994148
1995232
1996212
1997191
1998294
1999243
200063.0
2001244
2002106
2003136
2004195
2005159
2006121
2007367
2008420
2009297
2010600
2011290
201263.0
2013195
2014247
2015356
2016363
2017229
2018432
2019467
2020196
202195.0
2022105
202385.0
2024210
2025202

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 held1970–2025
Completeness100.0% of the periods in that span are held.
ContinuityContinuous: every year from 1970 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 Lower Des Moines and what each holds
GaugeMeasuresValuesRecord
Des Moines River at Ottumwa, IAburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2571903–2026
Des Moines River near Tracy, IAburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2531903–2026
Des Moines River at Keosauqua, IAcatchment area, annual maximum river flow, mean river flow, mean river flow, water year2321851–2026
Sugar Creek near Keokuk, IAcatchment area, annual maximum river flow251905–2026

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 — 07100009. 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
Des Moines River at Ottumwa, IAStated 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
Des Moines River near Tracy, IAStated 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
Des Moines River at Keosauqua, IAStated 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
Sugar Creek near Keokuk, IAStated 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 4 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 spanned176yes, 20 or more
Values held767no
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), Lower Des Moines gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-lower-des-moines/

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 Des Moines 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 confidence2025-08-08

Source: USGS — National Water Information System, USGS site 05489500, 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.