The monitoring network within this area

Hydrionis holds 377 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
377
Values held
1895–2026
Record spans
Gauges within the Middle Smoky Hill huc8 subbasin
2 monitoring points, positioned as the publisher records them.
Gauges within the Middle Smoky Hill huc8 subbasinSMOKY HILL R AT ELLSWORTH, KS, SMOKY HILL R AT PFEIFER, KSSMOKY HILL R AT ELLSWORTH, KSSMOKY HILL R AT PFEIFER, 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 AT ELLSWORTH, KS
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1895–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at SMOKY HILL R AT ELLSWORTH, KSLargest measured flow of each year at SMOKY HILL R AT ELLSWORTH, KS: SMOKY HILL R AT ELLSWORTH, KS in m³/s, from 1895 to 2025.Hurricane Katrina water and sanitation collapse05001,0001,5002,000m³/s18951922193819531968198419992014

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 AT ELLSWORTH, KS (m³/s)
1895736
1896129
189715.4
189831.1
1899351
190021.2
190118.7
1902351
1903527
1904248
1905188
1919142
192046.7
192168.2
1922365
1923223
192438.2
192572.5
19271,269
1928532
1929430
1930385
1932240
1933206
1934216
1935362
1936122
1937122
19381,727
1939258
1940133
1941518
1942481
1943109
1944365
1945371
1946161
1948107
1949311
1950377
1951850
1952314
195390.3
195499.4
1955306
1956115
1957394
1958289
1960510
1961527
1962428
1963116
1964141
1965328
1966206
1967498
1968188
1969422
1970603
1971345
1973501
1975286
1976132
1977213
197823.4
1979354
198096.8
1981197
1982189
19837.19
198472.5
1985328
198679.3
1987476
198810.2
1989106
1990682
1991189
1992345
1993858
199439.9
1995311
1996248
1998203
1999205
2000143
2001354
200237.7
2003101
200483.8
200532.3
200613.8
2007524
2008276
2010103
2011176
201219.8
201365.4
201474.5
201513.0
2016159
2017255
2018159
2020422
2021194
2022126
202319.3
2024292
2025142

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 held1895–2025
Completeness83.2% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 10 separate periods inside 1895–2025 hold no value. The longest runs from 1906 to 1918 — 13 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1895 and is not continuous from it: 131 years separate the first value from the last, and 83% 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 AT ELLSWORTH, 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. 1896–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above SMOKY HILL R AT ELLSWORTH, KS, as a depthWater leaving the catchment above SMOKY HILL R AT ELLSWORTH, KS, as a depth: SMOKY HILL R AT ELLSWORTH, KS in mm, from 1896 to 2025.Hurricane Katrina water and sanitation collapse020406080mm18961924194219561970198419982012

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 AT ELLSWORTH, KS (mm)
18965.00
18973.00
18983.00
18997.00
19004.00
19012.00
190218.0
190321.0
19048.00
191914.0
19203.00
19214.00
19226.00
192312.0
19244.00
192912.0
193014.0
19316.00
19329.00
193311.0
19345.00
193524.0
19365.00
19376.00
193822.0
19396.00
19405.00
194121.0
194216.0
19433.00
194417.0
19458.00
194613.0
19478.00
19487.00
194917.0
195027.0
195161.0
19529.00
19533.00
19543.00
19556.00
19562.00
195733.0
195825.0
195910.0
196022.0
196124.0
196217.0
19634.00
19644.00
196513.0
19667.00
196717.0
19686.00
196915.0
19709.00
197111.0
19725.00
197338.0
197414.0
19759.00
19764.00
19776.00
19783.00
19799.00
19805.00
19817.00
19825.00
19831.00
19844.00
19855.00
19863.00
198722.0
19882.00
19894.00
19907.00
19912.00
19928.00
199348.0
19945.00
199513.0
199611.0
19976.00
199815.0
199911.0
20006.00
200116.0
20023.00
20033.00
20043.00
20051.00
20061.00
200716.0
200816.0
20094.00
20106.00
20113.00
20121.00
20132.00
20144.00
20151.00
20166.00
20178.00
201817.0
201937.0
202012.0
202110.0
20224.00
20232.00
20252.00

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 held1896–2025
Completeness85.4% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 3 separate periods inside 1896–2025 hold no value. The longest runs from 1905 to 1918 — 14 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1896 and is not continuous from it: 130 years separate the first value from the last, and 85% 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 Middle Smoky Hill and what each holds
GaugeMeasuresValuesRecord
SMOKY HILL R AT ELLSWORTH, KScatchment area, annual maximum river flow, mean river flow, mean river flow, water year3411895–2026
SMOKY HILL R AT PFEIFER, KScatchment area, annual maximum river flow361970–2026

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 — 10260006. 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 AT ELLSWORTH, 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 PFEIFER, 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 record1no
Years spanned132yes, 20 or more
Values held377no
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), Middle Smoky Hill gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-middle-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 Middle 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 confidence2025-09-21

Source: USGS — National Water Information System, USGS site 06864500, 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.