The monitoring network within this area

Hydrionis holds 1,007 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
1,007
Values held
1902–2026
Record spans
Gauges within the Upper Clinch, Tennessee, Virginia huc8 subbasin
3 monitoring points, positioned as the publisher records them.
Gauges within the Upper Clinch, Tennessee, Virginia huc8 subbasinCLINCH RIVER ABOVE TAZEWELL, TN, CLINCH RIVER AT CLEVELAND, VA, CLINCH RIVER AT SPEERS FERRY, VACLINCH RIVER ABOVE TAZEWELL, TNCLINCH RIVER AT CLEVELAND, VACLINCH RIVER AT SPEERS FERRY, VA

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 CLINCH RIVER AT CLEVELAND, VA
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1902–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at CLINCH RIVER AT CLEVELAND, VALargest measured flow of each year at CLINCH RIVER AT CLEVELAND, VA: CLINCH RIVER AT CLEVELAND, VA in m³/s, from 1902 to 2025.Hurricane Katrina water and sanitation collapse02505007501,000m³/s19021932194719631978199320062019

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
PeriodCLINCH RIVER AT CLEVELAND, VA (m³/s)
1902631
1907631
1918609
1921194
1922273
1923464
1924323
1926236
1928147
1929251
1930157
1931236
1932331
1934244
1935323
1936294
1937248
1939297
1940637
1941170
1942204
1944515
1945281
1946436
1947430
1948385
1950442
1952191
1953453
1954198
1955439
1956396
1957878
1958394
1959222
1961405
1963770
1964195
1965331
1966206
1967388
1969130
1971464
1972388
1973580
1975521
1976161
1977977
1978600
1979459
1980175
1981133
1982229
1984530
1985283
1987377
198868.8
1989263
1990215
1991192
1993294
1994484
1995262
1996343
1997276
1998391
1999142
2000101
2001439
2002688
2003385
2004212
2006203
2007125
2008203
2009245
2011286
2012269
2013391
2014163
2015510
2016186
2017447
2018425
2019405
2020609
2021351
2022303
2023394
2024270
2025612

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 held1902–2025
Completeness73.4% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 20 separate periods inside 1902–2025 hold no value. The longest runs from 1908 to 1917 — 10 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1902 and is not continuous from it: 124 years separate the first value from the last, and 73% 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 CLINCH RIVER ABOVE TAZEWELL, TN, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1920–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above CLINCH RIVER ABOVE TAZEWELL, TN, as a depthWater leaving the catchment above CLINCH RIVER ABOVE TAZEWELL, TN, as a depth: CLINCH RIVER ABOVE TAZEWELL, TN in mm, from 1920 to 2025.Hurricane Katrina water and sanitation collapse200400600800mm19201934194819621976199020042018

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
PeriodCLINCH RIVER ABOVE TAZEWELL, TN (mm)
1920674
1921483
1922596
1923643
1924605
1925361
1926565
1927585
1928575
1929683
1930251
1931348
1932547
1933426
1934399
1935579
1936577
1937523
1938491
1939388
1940292
1941203
1942492
1943373
1944501
1945503
1946419
1947446
1948466
1949533
1950649
1951516
1952435
1953406
1954306
1955464
1956547
1957633
1958512
1959441
1960366
1961509
1962553
1963456
1964441
1965405
1966449
1967523
1968370
1969332
1970430
1971553
1972741
1973594
1974658
1975648
1976414
1977594
1978494
1979710
1980392
1981304
1982574
1983394
1984488
1985337
1986337
1987459
1988226
1989637
1990565
1991582
1992363
1993449
1994631
1995437
1996700
1997455
1998571
1999280
2000256
2001321
2002437
2003678
2004624
2005372
2006379
2007235
2008253
2009538
2010430
2011607
2012499
2013674
2014457
2015540
2016348
2017479
2018697
2019689
2020766
2021446
2022471
2023355
2024413
2025539

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 held1920–2025
Completeness100.0% of the periods in that span are held.
ContinuityContinuous: every year from 1920 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 Clinch, Tennessee, Virginia and what each holds
GaugeMeasuresValuesRecord
CLINCH RIVER AT CLEVELAND, VAburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3551902–2026
CLINCH RIVER ABOVE TAZEWELL, TNburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3521919–2026
CLINCH RIVER AT SPEERS FERRY, VAburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3001902–2026

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 — 06010205. 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
CLINCH RIVER AT CLEVELAND, VAStated 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
CLINCH RIVER ABOVE TAZEWELL, TNStated 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
CLINCH RIVER AT SPEERS FERRY, VAStated 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 5 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 spanned125yes, 20 or more
Values held1,007yes, 1000 or more
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 Clinch, Tennessee, Virginia gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-upper-clinch-tennessee-virginia/

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 Clinch, Tennessee, Virginia 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 confidence2025-02-16

Source: USGS — National Water Information System, USGS site 03524000, 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.