The monitoring network within this area

Hydrionis holds 804 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
804
Values held
1921–2026
Record spans
Gauges within the Cuyahoga huc8 subbasin
3 monitoring points, positioned as the publisher records them.
Gauges within the Cuyahoga huc8 subbasinCuyahoga River at Old Portage OH, Cuyahoga River at Independence OH, Cuyahoga River at Hiram Rapids OHCuyahoga River at Old Portage OHCuyahoga River at Independence OHCuyahoga River at Hiram Rapids 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 Cuyahoga River at Old Portage OH
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1922–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at Cuyahoga River at Old Portage OHLargest measured flow of each year at Cuyahoga River at Old Portage OH: Cuyahoga River at Old Portage OH in m³/s, from 1922 to 2025.Hurricane Katrina water and sanitation collapse050100150200m³/s19221935195019641977199220062018

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
PeriodCuyahoga River at Old Portage OH (m³/s)
192260.3
192352.1
1924126
192562.3
192679.9
192787.8
1929108
193092.9
193136.8
193248.7
1933101
193457.5
193577.9
193691.2
193977.9
194083.3
194186.1
194270.5
194475.9
194598.5
194665.1
194787.8
194879.6
194965.7
195088.3
1952129
195358.0
195456.6
195583.3
1957113
195885.0
1959184
196096.0
196192.9
196253.5
1963102
1964129
196564.0
196679.9
196760.6
196892.9
197082.1
197186.1
197292.9
197394.3
1974123
1975108
1976155
197771.4
1979176
198099.7
1981116
198297.1
198369.9
198481.6
1985101
198696.0
1988101
1989111
1990131
1992114
1993111
1994129
199589.2
1996107
199897.4
199965.7
200094.0
200277.0
2003146
2004158
2005129
2006104
2007117
2008125
2009101
201091.5
2011152
2012116
2013180
2014156
2015125
2016110
2017114
2018118
2019142
2020119
2021108
2022117
202394.3
2024136
2025102

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 held1922–2025
Completeness88.5% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 11 separate periods inside 1922–2025 hold no value. The longest runs from 1937 to 1938 — 2 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1922 and is not continuous from it: 104 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 Cuyahoga River at Old Portage 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. 1922–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above Cuyahoga River at Old Portage OH, as a depthWater leaving the catchment above Cuyahoga River at Old Portage OH, as a depth: Cuyahoga River at Old Portage OH in mm, from 1922 to 2025.Hurricane Katrina water and sanitation collapse0200400600800mm19221935195219651978199120042018

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
PeriodCuyahoga River at Old Portage OH (mm)
1922316
1923342
1924484
1925364
1926566
1927528
1928448
1929528
1930350
1931182
1932287
1933283
1934159
1935280
1940408
1941223
1942366
1943380
1944215
1945351
1946272
1947448
1948297
1949245
1950514
1951425
1952404
1953168
1954299
1955350
1956466
1957384
1958334
1959537
1960323
1961334
1962211
1963201
1964252
1965287
1966292
1967302
1968367
1969359
1970340
1971317
1972463
1973426
1974476
1975512
1976443
1977458
1978395
1979495
1980391
1981423
1982416
1983407
1984451
1985467
1986424
1987316
1988235
1989424
1990593
1991337
1992443
1993498
1994397
1995307
1996626
1997431
1998341
1999270
2000346
2001265
2002313
2003590
2004582
2005549
2006561
2007557
2008552
2009400
2010363
2011760
2012421
2013445
2014491
2015448
2016347
2018558
2019597
2020484
2021405
2022426
2023394
2024346
2025427

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 held1922–2025
Completeness95.2% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 2 separate periods inside 1922–2025 hold no value. The longest runs from 1936 to 1939 — 4 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1922 and is not continuous from it: 104 years separate the first value from the last, and 95% 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 Cuyahoga and what each holds
GaugeMeasuresValuesRecord
Cuyahoga River at Old Portage OHcatchment area, annual maximum river flow, mean river flow, mean river flow, water year3011921–2026
Cuyahoga River at Independence OHcatchment area, annual maximum river flow, mean river flow, mean river flow, water year2841921–2026
Cuyahoga River at Hiram Rapids OHcatchment area, annual maximum river flow, mean river flow, mean river flow, water year2191927–2026

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 — 04110002. 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
Cuyahoga River at Old Portage 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
Cuyahoga River at Independence 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
Cuyahoga River at Hiram Rapids 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 3 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 spanned106yes, 20 or more
Values held804no
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), Cuyahoga gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-cuyahoga/

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 Cuyahoga 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 confidence2025-04-05

Source: USGS — National Water Information System, USGS site 04206000, 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.