The monitoring network within this area

Hydrionis holds 1,028 values from 6 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.

6
Gauges
1,028
Values held
1884–2026
Record spans
Gauges within the Lower Kentucky huc8 subbasin
6 monitoring points, positioned as the publisher records them.
Gauges within the Lower Kentucky huc8 subbasinELKHORN CREEK NEAR FRANKFORT, KY, EAGLE CREEK AT GLENCOE, KY, KENTUCKY RIVER AT LOCK 10 NEAR WINCHESTER, KY, KENTUCKY RIVER AT LOCK 6 NEAR SALVISA, KY, KENTUCKY RIVER AT LOCK 4 AT FRANKFORT, KY, KENTUCKY RIVER AT LOCK 2 AT LOCKPORT, KYELKHORN CREEK NEAR FRANKFORT, KYEAGLE CREEK AT GLENCOE, KYKENTUCKY RIVER AT LOCK 10 NEAR WINCHESTER, KYKENTUCKY RIVER AT LOCK 6 NEAR SALVISA, KYKENTUCKY RIVER AT LOCK 4 AT FRANKFORT, KYKENTUCKY RIVER AT LOCK 2 AT LOCKPORT, KY

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 KENTUCKY RIVER AT LOCK 2 AT LOCKPORT, KY
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1884–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at KENTUCKY RIVER AT LOCK 2 AT LOCKPORT, KYLargest measured flow of each year at KENTUCKY RIVER AT LOCK 2 AT LOCKPORT, KY: KENTUCKY RIVER AT LOCK 2 AT LOCKPORT, KY in m³/s, from 1884 to 2025.Hurricane Katrina water and sanitation collapse01,0002,0003,0004,000m³/s18841901191919381955197219932011

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
PeriodKENTUCKY RIVER AT LOCK 2 AT LOCKPORT, KY (m³/s)
18841,951
18851,495
18862,135
18872,421
1888949
18900
18910
18921,623
18931,339
18941,209
18951,331
18961,416
18970
18980
18990
1900977
19011,727
19021,858
19041,068
19051,430
19061,617
19072,138
19082,189
19092,311
19101,724
19111,478
19121,829
19132,639
19141,396
19151,642
19172,203
19182,243
19192,209
1921906
19232,067
19242,353
19261,940
19272,390
19282,144
19292,067
19301,339
19311,271
19322,206
19331,699
19341,977
19352,257
19362,172
19373,483
19381,263
19392,478
19401,501
1941807
19421,455
19441,614
19452,659
19462,163
19471,492
19482,713
19492,149
19502,588
19511,974
19522,336
19531,767
1954555
19552,633
19562,234
19572,444
19581,872
19591,645
19601,756
19612,328
19622,917
19632,195
19642,860
19651,812
19661,334
19672,161
19681,787
1969937
19702,132
19722,945
19742,396
19752,495
19761,741
19771,625
19781,917
19791,320
19811,444
19821,586
19831,838
19842,645
19851,405
19871,623
19881,150
19893,455
19912,376
19931,719
19942,769
19952,427
19961,682
19972,832
19981,965
19991,557
20001,136
20032,384
20042,532
20051,487
20061,467
20071,116
20082,231
20091,654
20103,002
20112,059
20131,900
20141,880
20152,784
20171,008
20181,608
20192,254
20201,991
20212,798
20221,872
20231,917
20241,365
20253,511

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 held1884–2025
Completeness88.0% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 16 separate periods inside 1884–2025 hold no value. The longest runs from 2001 to 2002 — 2 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1884 and is not continuous from it: 142 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 ELKHORN CREEK NEAR FRANKFORT, 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. 1916–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above ELKHORN CREEK NEAR FRANKFORT, KY, as a depthWater leaving the catchment above ELKHORN CREEK NEAR FRANKFORT, KY, as a depth: ELKHORN CREEK NEAR FRANKFORT, KY in mm, from 1916 to 2025.Hurricane Katrina water and sanitation collapse05001,000mm19161949196019711982199720082019

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
PeriodELKHORN CREEK NEAR FRANKFORT, KY (mm)
1916502
1917523
1940359
1941139
1942625
1943479
1944210
1945630
1946430
1947401
1948736
1949571
1950901
1951777
1952438
1953389
1954129
1955493
1956580
1957596
1958509
1959431
1960627
1961753
1962620
1963343
1964543
1965399
1966495
1967491
1968496
1969320
1970614
1971432
1972790
1973600
1974805
1975832
1976350
1977397
1978774
1979850
1980346
1981301
1982453
1983653
1988368
1989843
1990795
1991692
1992580
1993631
1994706
1995591
1996889
1997800
1998673
1999309
2000393
2001442
2002759
2003785
2004989
2005358
2006587
2007499
2008669
2009705
2010440
20111,005
2012364
2013788
2014581
2015950
2016471
2017559
20181,212
2019887
2020602
2021793
2022540
2023410
2024559
20251,001

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 held1916–2025
Completeness76.4% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 2 separate periods inside 1916–2025 hold no value. The longest runs from 1918 to 1939 — 22 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1916 and is not continuous from it: 110 years separate the first value from the last, and 76% 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 Kentucky and what each holds
GaugeMeasuresValuesRecord
ELKHORN CREEK NEAR FRANKFORT, KYcatchment area, annual maximum river flow, mean river flow, mean river flow, water year2541915–2026
EAGLE CREEK AT GLENCOE, KYcatchment area, annual maximum river flow, mean river flow, mean river flow, water year2541915–2026
KENTUCKY RIVER AT LOCK 2 AT LOCKPORT, KYcatchment area, annual maximum river flow1401884–2026
KENTUCKY RIVER AT LOCK 6 NEAR SALVISA, KYcatchment area, annual maximum river flow1321895–2026
KENTUCKY RIVER AT LOCK 4 AT FRANKFORT, KYcatchment area, annual maximum river flow1301895–2026
KENTUCKY RIVER AT LOCK 10 NEAR WINCHESTER, KYcatchment area, annual maximum river flow1181908–2026

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 — 05100205. 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
ELKHORN CREEK NEAR FRANKFORT, 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/42026-10-02
EAGLE CREEK AT GLENCOE, 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/42026-10-02
KENTUCKY RIVER AT LOCK 2 AT LOCKPORT, 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/42026-10-02
KENTUCKY RIVER AT LOCK 6 NEAR SALVISA, 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/42026-10-02
KENTUCKY RIVER AT LOCK 4 AT FRANKFORT, 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/42026-10-02
KENTUCKY RIVER AT LOCK 10 NEAR WINCHESTER, 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/42026-10-02

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 record6yes, 3 or more
Years spanned143yes, 20 or more
Values held1,028yes, 1000 or more
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 Kentucky gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-lower-kentucky/

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 Kentucky 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 confidence2025-04-04

Source: USGS — National Water Information System, USGS site 03289500, 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.