The monitoring network within this area

Hydrionis holds 952 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
952
Values held
1897–2026
Record spans
Gauges within the Lower Gasconade huc8 subbasin
3 monitoring points, positioned as the publisher records them.
Gauges within the Lower Gasconade huc8 subbasinLittle Piney Creek at Newburg, MO, Gasconade River at Jerome, MO, Gasconade River near Rich Fountain, MOLittle Piney Creek at Newburg, MOGasconade River at Jerome, MOGasconade River near Rich Fountain, MO

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 Gasconade River at Jerome, MO
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1897–2024.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at Gasconade River at Jerome, MOLargest measured flow of each year at Gasconade River at Jerome, MO: Gasconade River at Jerome, MO in m³/s, from 1897 to 2024.Hurricane Katrina water and sanitation collapse02,0004,0006,000m³/s18971932194619611975198820052020

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
PeriodGasconade River at Jerome, MO (m³/s)
18973,398
1904960
19051,274
19153,228
1923439
1924861
1925394
19271,288
19281,730
1929926
1930830
1931212
1932314
19331,773
1934242
19352,175
1937765
19381,073
1939830
1940411
19411,546
1942895
1944354
19452,860
19462,478
19471,699
1948827
1949898
19501,379
19511,181
1953348
1955708
1956861
19571,625
19581,334
1959436
19611,778
1962694
1963779
1964711
1965796
19661,257
1967487
1968711
19691,368
1970643
1972787
19731,328
1975779
1976340
1977697
19781,087
19791,478
1980260
1981821
1982847
19841,291
19852,268
19861,540
19871,133
1988620
19901,464
1992408
19933,115
1995966
1996728
19981,147
1999883
2001861
20021,464
2003282
2004773
20051,070
2006852
2007436
20083,341
2009779
20112,410
20121,376
20133,908
20151,611
20175,578
20181,390
20191,178
20201,376
20211,099
20221,555
20231,699
20241,042

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 held1897–2024
Completeness69.5% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 20 separate periods inside 1897–2024 hold no value. The longest runs from 1906 to 1914 — 9 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1897 and is not continuous from it: 128 years separate the first value from the last, and 70% 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 Gasconade River at Jerome, MO, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1905–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above Gasconade River at Jerome, MO, as a depthWater leaving the catchment above Gasconade River at Jerome, MO, as a depth: Gasconade River at Jerome, MO in mm, from 1905 to 2025.Hurricane Katrina water and sanitation collapse0200400600800mm19051935194819611974198720002013

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
PeriodGasconade River at Jerome, MO (mm)
1905471
1923235
1924309
1925243
1926234
1927750
1928428
1929370
1930225
1931188
1932167
1933284
1934143
1935495
1936107
1937281
1938355
1939283
1940182
1941307
1942409
1943360
1944186
1945627
1946459
1947277
1948288
1949543
1950500
1951567
1952271
1953140
195480.0
1955165
1956118
1957426
1958356
1959240
1960189
1961340
1962223
1963163
1964120
1965224
1966300
1967279
1968319
1969286
1970303
1971206
1972252
1973533
1974423
1975378
1976127
1977179
1978249
1979403
1980157
1981206
1982416
1983449
1984512
1985780
1986297
1987310
1988326
1989231
1990490
1991340
1992271
1993600
1994428
1995425
1996403
1997290
1998376
1999289
200075.0
2001171
2002362
2003210
2004297
2005227
2006179
2007219
2008597
2009440
2010338
2011464
2012199
2013517
2014153
2015593
2016250
2017440
2018316
2019488
2020599
2021368
2022431
2023315
2024408
2025350

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 held1905–2025
Completeness86.0% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • One period inside 1905–2025 holds no value: 1906 to 1922, 17 years with no reading. It is drawn as a break in the line and is never interpolated across.
ContinuityThe record begins in 1905 and is not continuous from it: 121 years separate the first value from the last, and 86% 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

Every gauge Hydrionis holds within this area

Gauges within the Lower Gasconade and what each holds
GaugeMeasuresValuesRecord
Gasconade River at Jerome, MOburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3511897–2026
Little Piney Creek at Newburg, MOburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3281915–2026
Gasconade River near Rich Fountain, MOburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2731922–2026

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 — 10290203. 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
Gasconade River at Jerome, MOStated 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
Little Piney Creek at Newburg, MOStated 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
Gasconade River near Rich Fountain, MOStated 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 spanned130yes, 20 or more
Values held952no
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 Gasconade gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-lower-gasconade/

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 Gasconade 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 confidence2024-11-06

Source: USGS — National Water Information System, USGS site 06933500, 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.