The monitoring network within this area

Hydrionis holds 307 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
307
Values held
1903–2026
Record spans
Gauges within the Lower Smoky Hill huc8 subbasin
2 monitoring points, positioned as the publisher records them.
Gauges within the Lower Smoky Hill huc8 subbasinSMOKY HILL R NR MENTOR, KS, SMOKY HILL R AT LINDSBORG, KSSMOKY HILL R NR MENTOR, KSSMOKY HILL R AT LINDSBORG, KS

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 SMOKY HILL R NR MENTOR, KS
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1903–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at SMOKY HILL R NR MENTOR, KSLargest measured flow of each year at SMOKY HILL R NR MENTOR, KS: SMOKY HILL R NR MENTOR, KS in m³/s, from 1903 to 2025.Hurricane Katrina water and sanitation collapse02505007501,000m³/s19031948195819691981199220052016

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
PeriodSMOKY HILL R NR MENTOR, KS (m³/s)
1903906
192485.8
192559.5
1926107
1927722
1928368
1929368
1930119
193278.2
1938680
194899.4
1949294
1950317
1951566
1952227
195371.4
195464.6
1955195
1956113
1957108
1958113
195965.1
196087.2
1961121
196291.7
196376.7
196447.3
1965232
196648.1
1967183
1969188
1970104
1971167
1972190
1973292
1975151
197683.3
1977166
197851.0
1979116
1981144
1982202
198337.9
1984119
1985118
1987214
198834.8
198918.3
199061.4
199129.4
1992116
1993371
1995266
1996205
199893.2
2000222
2001102
200237.1
200364.3
200497.4
200558.6
20064.79
2007133
200856.1
2009152
201062.0
201118.3
2013158
201486.6
2015104
2016112
201752.4
201844.7
2019191
202060.6
202184.1
202252.7
202310.9
202439.6
2025126

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 held1903–2025
Completeness65.0% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 12 separate periods inside 1903–2025 hold no value. The longest runs from 1904 to 1923 — 20 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1903 and is not continuous from it: 123 years separate the first value from the last, and 65% 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 SMOKY HILL R NR MENTOR, KS, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1925–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above SMOKY HILL R NR MENTOR, KS, as a depthWater leaving the catchment above SMOKY HILL R NR MENTOR, KS, as a depth: SMOKY HILL R NR MENTOR, KS in mm, from 1925 to 2025.Hurricane Katrina water and sanitation collapse020406080mm19251954196519761987199820092020

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
PeriodSMOKY HILL R NR MENTOR, KS (mm)
19256.00
19264.00
192729.0
192822.0
192919.0
19488.00
194921.0
195030.0
195171.0
195213.0
19534.00
19543.00
19554.00
19562.00
195733.0
195827.0
195915.0
196027.0
196126.0
196220.0
19635.00
19644.00
196517.0
19668.00
196721.0
19687.00
196922.0
19709.00
197116.0
19729.00
197365.0
197427.0
197513.0
19767.00
197710.0
19786.00
197916.0
198010.0
198110.0
198211.0
19834.00
19847.00
198513.0
19866.00
198731.0
19884.00
19892.00
19906.00
19913.00
199210.0
199378.0
19948.00
199526.0
199619.0
199710.0
199826.0
199922.0
200012.0
200119.0
20024.00
20035.00
20044.00
20053.00
20061.00
200724.0
200821.0
20098.00
20107.00
20113.00
20121.00
20136.00
20146.00
20155.00
201610.0
201712.0
201817.0
201949.0
202015.0
202112.0
20226.00
20232.00
20242.00
20258.00

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 held1925–2025
Completeness82.2% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • One period inside 1925–2025 holds no value: 1930 to 1947, 18 years with no reading. It is drawn as a break in the line and is never interpolated across.
ContinuityThe record begins in 1925 and is not continuous from it: 101 years separate the first value from the last, and 82% 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 Smoky Hill and what each holds
GaugeMeasuresValuesRecord
SMOKY HILL R NR MENTOR, KScatchment area, annual maximum river flow, mean river flow, mean river flow, water year2571903–2026
SMOKY HILL R AT LINDSBORG, KScatchment area, annual maximum river flow501905–2026

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 — 10260008. 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
SMOKY HILL R NR MENTOR, KSStated 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
SMOKY HILL R AT LINDSBORG, KSStated 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 spanned124yes, 20 or more
Values held307no
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 Smoky Hill gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-lower-smoky-hill/

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 Smoky Hill 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 confidence2025-07-23

Source: USGS — National Water Information System, USGS site 06866500, 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.