The monitoring network within this area

Hydrionis holds 395 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
395
Values held
1898–2026
Record spans
Gauges within the Lower Scioto huc8 subbasin
2 monitoring points, positioned as the publisher records them.
Gauges within the Lower Scioto huc8 subbasinScioto River at Chillicothe OH, Deer Creek at Williamsport OHScioto River at Chillicothe OHDeer Creek at Williamsport OH

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 Scioto River at Chillicothe OH
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1898–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at Scioto River at Chillicothe OHLargest measured flow of each year at Scioto River at Chillicothe OH: Scioto River at Chillicothe OH in m³/s, from 1898 to 2025.Hurricane Katrina water and sanitation collapse02,0004,0006,0008,000m³/s18981921193719511965197919942009

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
PeriodScioto River at Chillicothe OH (m³/s)
18980
19081,659
19092,132
19102,653
1911943
19121,164
19137,362
1914770
19151,076
19161,886
1917847
19181,192
19191,090
19201,815
19211,705
19221,362
1923592
19241,719
1925430
1926895
19271,693
19292,512
19301,410
1931481
19332,401
1934371
1935651
19361,348
19372,860
19381,337
1939974
19401,999
1941464
1942917
19431,979
1944895
19452,367
19461,121
19471,447
19481,744
19491,093
19501,362
19511,246
19522,418
1953311
1954340
1955787
1956617
19571,557
1958980
19594,078
1960606
1961818
19621,002
19632,180
19642,248
1965762
1966626
1967796
19681,104
1969799
1970940
1971756
1972733
1973762
1974796
19751,617
1976875
1977583
1978983
19791,152
1980895
1981869
1982827
1983991
1984980
1985923
1986697
1988691
1989784
19901,000
19911,399
1992702
1993745
19941,042
1995733
19961,085
19971,192
1998807
1999597
2000779
2001674
2003694
20041,461
20051,917
2006762
20071,017
20081,223
2009668
2010745
20111,036
2013583
2015977
2017722
20181,254
20191,138
20201,240
2021736
20221,079
2023881
20241,277
20251,169

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 held1898–2025
Completeness87.5% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 8 separate periods inside 1898–2025 hold no value. The longest runs from 1899 to 1907 — 9 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1898 and is not continuous from it: 128 years separate the first value from the last, and 88% 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 Scioto River at Chillicothe OH, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1921–2024.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above Scioto River at Chillicothe OH, as a depthWater leaving the catchment above Scioto River at Chillicothe OH, as a depth: Scioto River at Chillicothe OH in mm, from 1921 to 2024.Hurricane Katrina water and sanitation collapse0200400600800mm19211934194719601973198619992012

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
PeriodScioto River at Chillicothe OH (mm)
1921414
1922318
1923309
1924329
1925151
1926367
1927465
1928287
1929506
1930279
1931203
1932259
1933373
193472.0
1935219
1936242
1937460
1938298
1939296
1940273
1941120
1942210
1943312
1944167
1945374
1946267
1947435
1948396
1949324
1950473
1951379
1952350
1953124
195493.0
1955207
1956273
1957344
1958340
1959329
1960174
1961310
1962236
1963224
1964281
1965234
1966278
1967312
1968307
1969346
1970332
1971245
1972481
1973480
1974377
1975395
1976256
1977261
1978359
1979542
1980404
1981327
1982336
1983302
1984327
1985361
1986379
1987224
1988212
1989455
1990614
1991306
1992276
1993414
1994271
1995393
1996579
1997346
1998334
1999230
2000287
2001284
2002296
2003512
2004487
2005503
2006401
2007425
2008485
2009246
2010280
2011717
2012287
2013407
2014365
2015424
2016315
2017450
2018619
2019575
2020449
2021341
2022437
2023304
2024307

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 held1921–2024
Completeness100.0% of the periods in that span are held.
ContinuityContinuous: every year from 1921 to 2024 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 Scioto and what each holds
GaugeMeasuresValuesRecord
Scioto River at Chillicothe OHcatchment area, annual maximum river flow, mean river flow, mean river flow, water year3291898–2026
Deer Creek at Williamsport OHcatchment area, annual maximum river flow661927–2026

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 — 05060002. 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
Scioto River at Chillicothe OHStated 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
Deer Creek at Williamsport OHStated 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 2 of them, which makes it a profile, not indexed.

Information-gain signals held for this water body
SignalHeldCounts
Gauges holding a real record2no
Years spanned129yes, 20 or more
Values held395no
Distinct measurements4yes, 2 or more
Publishers measuring it1no
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 Scioto gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-lower-scioto/

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 Scioto 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 confidence2025-04-08

Source: USGS — National Water Information System, USGS site 03231500, 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.