The monitoring network within this area

Hydrionis holds 366 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
366
Values held
1890–2026
Record spans
Gauges within the Kentucky Lake huc8 subbasin
2 monitoring points, positioned as the publisher records them.
Gauges within the Kentucky Lake huc8 subbasinTENNESSEE RIVER NEAR PADUCAH, KY, BIG SANDY RIVER AT BRUCETON, TNTENNESSEE RIVER NEAR PADUCAH, KYBIG SANDY RIVER AT BRUCETON, TN

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 BIG SANDY RIVER AT BRUCETON, TN
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1930–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at BIG SANDY RIVER AT BRUCETON, TNLargest measured flow of each year at BIG SANDY RIVER AT BRUCETON, TN: BIG SANDY RIVER AT BRUCETON, TN in m³/s, from 1930 to 2025.Hurricane Katrina water and sanitation collapse0200400m³/s19301940194919621972198220092022BIG SANDY RIVER AT BRUCETON, TN 1930: 258 m³/sBIG SANDY RIVER AT BRUCETON, TN 1931: 58.3 m³/sBIG SANDY RIVER AT BRUCETON, TN 1932: 221 m³/sBIG SANDY RIVER AT BRUCETON, TN 1933: 91.2 m³/sBIG SANDY RIVER AT BRUCETON, TN 1933: 158 m³/sBIG SANDY RIVER AT BRUCETON, TN 1935: 481 m³/sBIG SANDY RIVER AT BRUCETON, TN 1936: 191 m³/sBIG SANDY RIVER AT BRUCETON, TN 1937: 391 m³/sBIG SANDY RIVER AT BRUCETON, TN 1938: 121 m³/sBIG SANDY RIVER AT BRUCETON, TN 1939: 168 m³/sBIG SANDY RIVER AT BRUCETON, TN 1940: 47.6 m³/sBIG SANDY RIVER AT BRUCETON, TN 1941: 34.0 m³/sBIG SANDY RIVER AT BRUCETON, TN 1942: 286 m³/sBIG SANDY RIVER AT BRUCETON, TN 1943: 107 m³/sBIG SANDY RIVER AT BRUCETON, TN 1944: 151 m³/sBIG SANDY RIVER AT BRUCETON, TN 1945: 159 m³/sBIG SANDY RIVER AT BRUCETON, TN 1946: 340 m³/sBIG SANDY RIVER AT BRUCETON, TN 1947: 113 m³/sBIG SANDY RIVER AT BRUCETON, TN 1948: 174 m³/sBIG SANDY RIVER AT BRUCETON, TN 1948: 134 m³/sBIG SANDY RIVER AT BRUCETON, TN 1949: 280 m³/sBIG SANDY RIVER AT BRUCETON, TN 1951: 148 m³/sBIG SANDY RIVER AT BRUCETON, TN 1951: 121 m³/sBIG SANDY RIVER AT BRUCETON, TN 1953: 142 m³/sBIG SANDY RIVER AT BRUCETON, TN 1954: 94.0 m³/sBIG SANDY RIVER AT BRUCETON, TN 1955: 155 m³/sBIG SANDY RIVER AT BRUCETON, TN 1956: 334 m³/sBIG SANDY RIVER AT BRUCETON, TN 1957: 146 m³/sBIG SANDY RIVER AT BRUCETON, TN 1957: 94.9 m³/sBIG SANDY RIVER AT BRUCETON, TN 1959: 68.0 m³/sBIG SANDY RIVER AT BRUCETON, TN 1959: 41.3 m³/sBIG SANDY RIVER AT BRUCETON, TN 1961: 107 m³/sBIG SANDY RIVER AT BRUCETON, TN 1962: 212 m³/sBIG SANDY RIVER AT BRUCETON, TN 1963: 77.6 m³/sBIG SANDY RIVER AT BRUCETON, TN 1964: 87.8 m³/sBIG SANDY RIVER AT BRUCETON, TN 1965: 203 m³/sBIG SANDY RIVER AT BRUCETON, TN 1966: 54.4 m³/sBIG SANDY RIVER AT BRUCETON, TN 1967: 257 m³/sBIG SANDY RIVER AT BRUCETON, TN 1968: 87.2 m³/sBIG SANDY RIVER AT BRUCETON, TN 1968: 79.3 m³/sBIG SANDY RIVER AT BRUCETON, TN 1970: 123 m³/sBIG SANDY RIVER AT BRUCETON, TN 1971: 144 m³/sBIG SANDY RIVER AT BRUCETON, TN 1972: 340 m³/sBIG SANDY RIVER AT BRUCETON, TN 1973: 216 m³/sBIG SANDY RIVER AT BRUCETON, TN 1974: 244 m³/sBIG SANDY RIVER AT BRUCETON, TN 1975: 357 m³/sBIG SANDY RIVER AT BRUCETON, TN 1976: 83.3 m³/sBIG SANDY RIVER AT BRUCETON, TN 1977: 98.0 m³/sBIG SANDY RIVER AT BRUCETON, TN 1978: 74.2 m³/sBIG SANDY RIVER AT BRUCETON, TN 1979: 267 m³/sBIG SANDY RIVER AT BRUCETON, TN 1979: 190 m³/sBIG SANDY RIVER AT BRUCETON, TN 1981: 110 m³/sBIG SANDY RIVER AT BRUCETON, TN 1982: 111 m³/sBIG SANDY RIVER AT BRUCETON, TN 1982: 129 m³/sBIG SANDY RIVER AT BRUCETON, TN 1984: 142 m³/sBIG SANDY RIVER AT BRUCETON, TN 1984: 54.1 m³/sBIG SANDY RIVER AT BRUCETON, TN 1986: 36.5 m³/sBIG SANDY RIVER AT BRUCETON, TN 1986: 85.0 m³/sBIG SANDY RIVER AT BRUCETON, TN 2002: 259 m³/sBIG SANDY RIVER AT BRUCETON, TN 2004: 67.4 m³/sBIG SANDY RIVER AT BRUCETON, TN 2005: 62.3 m³/sBIG SANDY RIVER AT BRUCETON, TN 2006: 166 m³/sBIG SANDY RIVER AT BRUCETON, TN 2007: 51.8 m³/sBIG SANDY RIVER AT BRUCETON, TN 2008: 87.5 m³/sBIG SANDY RIVER AT BRUCETON, TN 2009: 360 m³/sBIG SANDY RIVER AT BRUCETON, TN 2011: 186 m³/sBIG SANDY RIVER AT BRUCETON, TN 2011: 83.5 m³/sBIG SANDY RIVER AT BRUCETON, TN 2013: 95.1 m³/sBIG SANDY RIVER AT BRUCETON, TN 2014: 176 m³/sBIG SANDY RIVER AT BRUCETON, TN 2015: 161 m³/sBIG SANDY RIVER AT BRUCETON, TN 2016: 152 m³/sBIG SANDY RIVER AT BRUCETON, TN 2017: 128 m³/sBIG SANDY RIVER AT BRUCETON, TN 2017: 170 m³/sBIG SANDY RIVER AT BRUCETON, TN 2019: 274 m³/sBIG SANDY RIVER AT BRUCETON, TN 2019: 160 m³/sBIG SANDY RIVER AT BRUCETON, TN 2021: 186 m³/sBIG SANDY RIVER AT BRUCETON, TN 2022: 92.6 m³/sBIG SANDY RIVER AT BRUCETON, TN 2023: 59.5 m³/sBIG SANDY RIVER AT BRUCETON, TN 2024: 51.3 m³/sBIG SANDY RIVER AT BRUCETON, TN 2025: 331 m³/s

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 recordA 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 collapseFlood2005-08-292005-09-30Documented record
Compiled record

Not shown on this chart

  • The 1976 droughtThis 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 droughtThis event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • Yorkshire droughtThis 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 PauloThis 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 ZeroThis event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • European droughtThis 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
PeriodBIG SANDY RIVER AT BRUCETON, TN (m³/s)
1930258
193158.3
1932221
193391.2
1935481
1936191
1937391
1938121
1939168
194047.6
194134.0
1942286
1943107
1944151
1945159
1946340
1947113
1948174
1949280
1951148
1953142
195494.0
1955155
1956334
1957146
195968.0
1961107
1962212
196377.6
196487.8
1965203
196654.4
1967257
196887.2
1970123
1971144
1972340
1973216
1974244
1975357
197683.3
197798.0
197874.2
1979267
1981110
1982111
1984142
198636.5
2002259
200467.4
200562.3
2006166
200751.8
200887.5
2009360
2011186
201395.1
2014176
2015161
2016152
2017128
2019274
2021186
202292.6
202359.5
202451.3
2025331

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 held19302025
Completeness69.8% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 15 separate periods inside 1930–2025 hold no value. The longest runs from 1987 to 2001 — 15 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1930 and is not continuous from it: 96 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 publisher2026-08-31
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 TENNESSEE RIVER NEAR PADUCAH, KY, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1890–1983.
Water leaving the catchment above TENNESSEE RIVER NEAR PADUCAH, KY, as a depthWater leaving the catchment above TENNESSEE RIVER NEAR PADUCAH, KY, as a depth: TENNESSEE RIVER NEAR PADUCAH, KY in mm, from 1890 to 1983.2004006008001,000mm18901902191419261938195019621974

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 (0 events)

Not shown on this chart

  • The 1976 droughtThis 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 droughtThis event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • Yorkshire droughtThis 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 PauloThis 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 ZeroThis event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • European droughtThis 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
PeriodTENNESSEE RIVER NEAR PADUCAH, KY (mm)
1890626
1891692
1892649
1893568
1894378
1895411
1896426
1897581
1898418
1899605
1900521
1901605
1902563
1903575
1904274
1905464
1906594
1907513
1908519
1909670
1910416
1911546
1912666
1913558
1914330
1915520
1916564
1917644
1918499
1919644
1920769
1921519
1922672
1923675
1924557
1925324
1926448
1927680
1928634
1929804
1930378
1931359
1932713
1933618
1934434
1935556
1936566
1937617
1938507
1939547
1940361
1941268
1942395
1943489
1944535
1945601
1946688
1947525
1948660
1949729
1950786
1951697
1952488
1953505
1954418
1955517
1956515
1957775
1958535
1959477
1960494
1961638
1962698
1963500
1964673
1965549
1966413
1967576
1968459
1969427
1970484
1971524
1972640
1973810
1974745
1975754
1976439
1977599
1978473
1979778
1980529
1981306
1982584
1983635

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 held18901983
Completeness100.0% of the periods in that span are held.
ContinuityContinuous: every year from 1890 to 1983 is held.
Last read from the publisher2026-08-24
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 Kentucky Lake and what each holds
GaugeMeasuresValuesRecord
BIG SANDY RIVER AT BRUCETON, TNburned area within 50 km, catchment area, annual maximum river flow, mean river flow1951930–2026
TENNESSEE RIVER NEAR PADUCAH, KYburned area within 50 km, catchment area, annual maximum river flow, mean river flow1711890–2026

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 — 06040005. 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
BIG SANDY RIVER AT BRUCETON, 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/42026-08-26
TENNESSEE RIVER NEAR PADUCAH, KYStated 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/42026-08-26

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 record2no
Years spanned137yes, 20 or more
Values held366no
Distinct measurements4yes, 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), Kentucky Lake gauge records, accessed 2026-09-02, hydrionis.com/waters/united-states-kentucky-lake/

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 Kentucky Lake 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 confidence2025-04-06

Source: USGSNational Water Information System, USGS site 03606500, 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 31 August 2026.