The monitoring network within this area

Hydrionis holds 1,100 values from 5 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.

5
Gauges
1,100
Values held
1910–2026
Record spans
Gauges within the Warner Lakes huc8 subbasin
5 monitoring points, positioned as the publisher records them.
Gauges within the Warner Lakes huc8 subbasinTWENTYMILE CREEK NEAR ADEL,OREG., DEEP CREEK ABOVE ADEL,OREG., CAMAS CREEK NEAR LAKEVIEW,OREG., DRAKE CREEK NEAR ADEL,OREG., HONEY CREEK NEAR PLUSH,OREG.TWENTYMILE CREEK NEAR ADEL,OREG.DEEP CREEK ABOVE ADEL,OREG.CAMAS CREEK NEAR LAKEVIEW,OREG.DRAKE CREEK NEAR ADEL,OREG.HONEY CREEK NEAR PLUSH,OREG.

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 HONEY CREEK NEAR PLUSH,OREG.
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1910–1991.
Largest measured flow of each year at HONEY CREEK NEAR PLUSH,OREG.Largest measured flow of each year at HONEY CREEK NEAR PLUSH,OREG.: HONEY CREEK NEAR PLUSH,OREG. in m³/s, from 1910 to 1991.0100200300400m³/s19101931194019491958196819771987HONEY CREEK NEAR PLUSH,OREG. 1910: 63.4 m³/sHONEY CREEK NEAR PLUSH,OREG. 1911: 41.3 m³/sHONEY CREEK NEAR PLUSH,OREG. 1912: 9.17 m³/sHONEY CREEK NEAR PLUSH,OREG. 1913: 26.9 m³/sHONEY CREEK NEAR PLUSH,OREG. 1914: 13.2 m³/sHONEY CREEK NEAR PLUSH,OREG. 1915: 109 m³/sHONEY CREEK NEAR PLUSH,OREG. 1921: 8.16 m³/sHONEY CREEK NEAR PLUSH,OREG. 1922: 13.9 m³/sHONEY CREEK NEAR PLUSH,OREG. 1930: 2.10 m³/sHONEY CREEK NEAR PLUSH,OREG. 1931: 0.821 m³/sHONEY CREEK NEAR PLUSH,OREG. 1932: 9.32 m³/sHONEY CREEK NEAR PLUSH,OREG. 1933: 3.40 m³/sHONEY CREEK NEAR PLUSH,OREG. 1934: 1.27 m³/sHONEY CREEK NEAR PLUSH,OREG. 1935: 5.83 m³/sHONEY CREEK NEAR PLUSH,OREG. 1936: 6.00 m³/sHONEY CREEK NEAR PLUSH,OREG. 1937: 10.9 m³/sHONEY CREEK NEAR PLUSH,OREG. 1938: 24.7 m³/sHONEY CREEK NEAR PLUSH,OREG. 1939: 8.13 m³/sHONEY CREEK NEAR PLUSH,OREG. 1940: 21.4 m³/sHONEY CREEK NEAR PLUSH,OREG. 1941: 8.33 m³/sHONEY CREEK NEAR PLUSH,OREG. 1942: 19.9 m³/sHONEY CREEK NEAR PLUSH,OREG. 1943: 17.5 m³/sHONEY CREEK NEAR PLUSH,OREG. 1944: 26.6 m³/sHONEY CREEK NEAR PLUSH,OREG. 1945: 12.8 m³/sHONEY CREEK NEAR PLUSH,OREG. 1946: 10.9 m³/sHONEY CREEK NEAR PLUSH,OREG. 1947: 3.65 m³/sHONEY CREEK NEAR PLUSH,OREG. 1948: 39.1 m³/sHONEY CREEK NEAR PLUSH,OREG. 1949: 12.8 m³/sHONEY CREEK NEAR PLUSH,OREG. 1950: 5.49 m³/sHONEY CREEK NEAR PLUSH,OREG. 1951: 24.1 m³/sHONEY CREEK NEAR PLUSH,OREG. 1952: 42.2 m³/sHONEY CREEK NEAR PLUSH,OREG. 1953: 16.4 m³/sHONEY CREEK NEAR PLUSH,OREG. 1954: 7.11 m³/sHONEY CREEK NEAR PLUSH,OREG. 1955: 9.06 m³/sHONEY CREEK NEAR PLUSH,OREG. 1956: 30.0 m³/sHONEY CREEK NEAR PLUSH,OREG. 1957: 20.4 m³/sHONEY CREEK NEAR PLUSH,OREG. 1958: 13.0 m³/sHONEY CREEK NEAR PLUSH,OREG. 1959: 2.61 m³/sHONEY CREEK NEAR PLUSH,OREG. 1960: 11.8 m³/sHONEY CREEK NEAR PLUSH,OREG. 1961: 2.49 m³/sHONEY CREEK NEAR PLUSH,OREG. 1962: 8.41 m³/sHONEY CREEK NEAR PLUSH,OREG. 1963: 176 m³/sHONEY CREEK NEAR PLUSH,OREG. 1964: 24.5 m³/sHONEY CREEK NEAR PLUSH,OREG. 1964: 311 m³/sHONEY CREEK NEAR PLUSH,OREG. 1966: 3.06 m³/sHONEY CREEK NEAR PLUSH,OREG. 1967: 25.6 m³/sHONEY CREEK NEAR PLUSH,OREG. 1968: 3.11 m³/sHONEY CREEK NEAR PLUSH,OREG. 1969: 23.9 m³/sHONEY CREEK NEAR PLUSH,OREG. 1970: 23.7 m³/sHONEY CREEK NEAR PLUSH,OREG. 1971: 27.6 m³/sHONEY CREEK NEAR PLUSH,OREG. 1972: 24.3 m³/sHONEY CREEK NEAR PLUSH,OREG. 1973: 5.41 m³/sHONEY CREEK NEAR PLUSH,OREG. 1974: 34.3 m³/sHONEY CREEK NEAR PLUSH,OREG. 1975: 22.3 m³/sHONEY CREEK NEAR PLUSH,OREG. 1976: 4.13 m³/sHONEY CREEK NEAR PLUSH,OREG. 1977: 1.02 m³/sHONEY CREEK NEAR PLUSH,OREG. 1978: 17.6 m³/sHONEY CREEK NEAR PLUSH,OREG. 1979: 13.5 m³/sHONEY CREEK NEAR PLUSH,OREG. 1980: 21.2 m³/sHONEY CREEK NEAR PLUSH,OREG. 1981: 6.17 m³/sHONEY CREEK NEAR PLUSH,OREG. 1981: 67.7 m³/sHONEY CREEK NEAR PLUSH,OREG. 1983: 26.3 m³/sHONEY CREEK NEAR PLUSH,OREG. 1984: 14.7 m³/sHONEY CREEK NEAR PLUSH,OREG. 1985: 10.6 m³/sHONEY CREEK NEAR PLUSH,OREG. 1986: 31.4 m³/sHONEY CREEK NEAR PLUSH,OREG. 1987: 3.26 m³/sHONEY CREEK NEAR PLUSH,OREG. 1988: 4.13 m³/sHONEY CREEK NEAR PLUSH,OREG. 1989: 10.6 m³/sHONEY CREEK NEAR PLUSH,OREG. 1990: 7.48 m³/sHONEY CREEK NEAR PLUSH,OREG. 1991: 14.1 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 (0 events)

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
PeriodHONEY CREEK NEAR PLUSH,OREG. (m³/s)
191063.4
191141.3
19129.17
191326.9
191413.2
1915109
19218.16
192213.9
19302.10
19310.821
19329.32
19333.40
19341.27
19355.83
19366.00
193710.9
193824.7
19398.13
194021.4
19418.33
194219.9
194317.5
194426.6
194512.8
194610.9
19473.65
194839.1
194912.8
19505.49
195124.1
195242.2
195316.4
19547.11
19559.06
195630.0
195720.4
195813.0
19592.61
196011.8
19612.49
19628.41
1963176
196424.5
19663.06
196725.6
19683.11
196923.9
197023.7
197127.6
197224.3
19735.41
197434.3
197522.3
19764.13
19771.02
197817.6
197913.5
198021.2
19816.17
198326.3
198414.7
198510.6
198631.4
19873.26
19884.13
198910.6
19907.48
199114.1

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 held1910–1991
Completeness82.9% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 4 separate periods inside 1910–1991 hold no value. The longest runs from 1923 to 1929 — 7 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1910 and is not continuous from it: 82 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 DEEP CREEK ABOVE ADEL,OREG., as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1933–1990.
Water leaving the catchment above DEEP CREEK ABOVE ADEL,OREG., as a depthWater leaving the catchment above DEEP CREEK ABOVE ADEL,OREG., as a depth: DEEP CREEK ABOVE ADEL,OREG. in mm, from 1933 to 1990.0100200300400mm19331941194919571965197319811989DEEP CREEK ABOVE ADEL,OREG. 1933: 66.0 mmDEEP CREEK ABOVE ADEL,OREG. 1934: 42.0 mmDEEP CREEK ABOVE ADEL,OREG. 1935: 162 mmDEEP CREEK ABOVE ADEL,OREG. 1936: 163 mmDEEP CREEK ABOVE ADEL,OREG. 1937: 142 mmDEEP CREEK ABOVE ADEL,OREG. 1938: 257 mmDEEP CREEK ABOVE ADEL,OREG. 1939: 81.0 mmDEEP CREEK ABOVE ADEL,OREG. 1940: 136 mmDEEP CREEK ABOVE ADEL,OREG. 1941: 144 mmDEEP CREEK ABOVE ADEL,OREG. 1942: 215 mmDEEP CREEK ABOVE ADEL,OREG. 1943: 311 mmDEEP CREEK ABOVE ADEL,OREG. 1944: 108 mmDEEP CREEK ABOVE ADEL,OREG. 1945: 187 mmDEEP CREEK ABOVE ADEL,OREG. 1946: 157 mmDEEP CREEK ABOVE ADEL,OREG. 1947: 91.0 mmDEEP CREEK ABOVE ADEL,OREG. 1948: 175 mmDEEP CREEK ABOVE ADEL,OREG. 1949: 161 mmDEEP CREEK ABOVE ADEL,OREG. 1950: 208 mmDEEP CREEK ABOVE ADEL,OREG. 1951: 207 mmDEEP CREEK ABOVE ADEL,OREG. 1952: 303 mmDEEP CREEK ABOVE ADEL,OREG. 1953: 245 mmDEEP CREEK ABOVE ADEL,OREG. 1954: 168 mmDEEP CREEK ABOVE ADEL,OREG. 1955: 151 mmDEEP CREEK ABOVE ADEL,OREG. 1956: 321 mmDEEP CREEK ABOVE ADEL,OREG. 1957: 217 mmDEEP CREEK ABOVE ADEL,OREG. 1958: 289 mmDEEP CREEK ABOVE ADEL,OREG. 1959: 72.0 mmDEEP CREEK ABOVE ADEL,OREG. 1960: 123 mmDEEP CREEK ABOVE ADEL,OREG. 1961: 94.0 mmDEEP CREEK ABOVE ADEL,OREG. 1962: 187 mmDEEP CREEK ABOVE ADEL,OREG. 1963: 220 mmDEEP CREEK ABOVE ADEL,OREG. 1964: 211 mmDEEP CREEK ABOVE ADEL,OREG. 1965: 283 mmDEEP CREEK ABOVE ADEL,OREG. 1966: 108 mmDEEP CREEK ABOVE ADEL,OREG. 1967: 200 mmDEEP CREEK ABOVE ADEL,OREG. 1968: 84.0 mmDEEP CREEK ABOVE ADEL,OREG. 1969: 243 mmDEEP CREEK ABOVE ADEL,OREG. 1970: 252 mmDEEP CREEK ABOVE ADEL,OREG. 1971: 385 mmDEEP CREEK ABOVE ADEL,OREG. 1972: 306 mmDEEP CREEK ABOVE ADEL,OREG. 1973: 161 mmDEEP CREEK ABOVE ADEL,OREG. 1974: 279 mmDEEP CREEK ABOVE ADEL,OREG. 1975: 227 mmDEEP CREEK ABOVE ADEL,OREG. 1976: 132 mmDEEP CREEK ABOVE ADEL,OREG. 1977: 52.0 mmDEEP CREEK ABOVE ADEL,OREG. 1978: 204 mmDEEP CREEK ABOVE ADEL,OREG. 1979: 121 mmDEEP CREEK ABOVE ADEL,OREG. 1980: 230 mmDEEP CREEK ABOVE ADEL,OREG. 1981: 163 mmDEEP CREEK ABOVE ADEL,OREG. 1982: 324 mmDEEP CREEK ABOVE ADEL,OREG. 1983: 345 mmDEEP CREEK ABOVE ADEL,OREG. 1984: 310 mmDEEP CREEK ABOVE ADEL,OREG. 1985: 163 mmDEEP CREEK ABOVE ADEL,OREG. 1986: 271 mmDEEP CREEK ABOVE ADEL,OREG. 1987: 97.0 mmDEEP CREEK ABOVE ADEL,OREG. 1988: 88.0 mmDEEP CREEK ABOVE ADEL,OREG. 1989: 235 mmDEEP CREEK ABOVE ADEL,OREG. 1990: 66.0 mm

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 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
PeriodDEEP CREEK ABOVE ADEL,OREG. (mm)
193366.0
193442.0
1935162
1936163
1937142
1938257
193981.0
1940136
1941144
1942215
1943311
1944108
1945187
1946157
194791.0
1948175
1949161
1950208
1951207
1952303
1953245
1954168
1955151
1956321
1957217
1958289
195972.0
1960123
196194.0
1962187
1963220
1964211
1965283
1966108
1967200
196884.0
1969243
1970252
1971385
1972306
1973161
1974279
1975227
1976132
197752.0
1978204
1979121
1980230
1981163
1982324
1983345
1984310
1985163
1986271
198797.0
198888.0
1989235
199066.0

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 held1933–1990
Completeness100.0% of the periods in that span are held.
ContinuityContinuous: every year from 1933 to 1990 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

The snow standing above this water

1 automated snow station sits inside this drainage area, weighing the snowpack rather than measuring how deep it is.

1,205
Fullest snowpack recorded at Dismal Swamp, in 2017 (mm of water)
258
Thinnest, in 2026 (mm of water)
April
Month the pack is usually at its fullest
June
Month the pack has gone by, in half of years
Peak snowpack at Dismal Swamp
Water years 1981–2026. Each point is the fullest month of that snow season.
Peak snowpack at Dismal SwampPeak snowpack at Dismal Swamp: Dismal Swamp in mm, from 1981 to 2026.05001,000mm19811987199319992005201120172023Dismal Swamp 1981: 489 mmDismal Swamp 1982: 900 mmDismal Swamp 1983: 1,117 mmDismal Swamp 1984: 945 mmDismal Swamp 1985: 700 mmDismal Swamp 1986: 757 mmDismal Swamp 1987: 504 mmDismal Swamp 1988: 427 mmDismal Swamp 1989: 885 mmDismal Swamp 1990: 454 mmDismal Swamp 1991: 554 mmDismal Swamp 1992: 324 mmDismal Swamp 1993: 942 mmDismal Swamp 1994: 385 mmDismal Swamp 1995: 778 mmDismal Swamp 1996: 765 mmDismal Swamp 1997: 871 mmDismal Swamp 1998: 1,062 mmDismal Swamp 1999: 1,051 mmDismal Swamp 2000: 745 mmDismal Swamp 2001: 467 mmDismal Swamp 2002: 831 mmDismal Swamp 2003: 668 mmDismal Swamp 2004: 805 mmDismal Swamp 2005: 747 mmDismal Swamp 2006: 1,198 mmDismal Swamp 2007: 525 mmDismal Swamp 2008: 705 mmDismal Swamp 2009: 688 mmDismal Swamp 2010: 668 mmDismal Swamp 2011: 1,150 mmDismal Swamp 2012: 487 mmDismal Swamp 2013: 511 mmDismal Swamp 2014: 392 mmDismal Swamp 2015: 341 mmDismal Swamp 2016: 850 mmDismal Swamp 2017: 1,205 mmDismal Swamp 2018: 569 mmDismal Swamp 2019: 1,090 mmDismal Swamp 2020: 706 mmDismal Swamp 2021: 592 mmDismal Swamp 2022: 510 mmDismal Swamp 2023: 1,110 mmDismal Swamp 2024: 877 mmDismal Swamp 2025: 1,072 mmDismal Swamp 2026: 258 mm

A water year runs October to September and is named for the year it ends, so the snow of one winter stays in one point. The value is the fullest month, not the fullest day: a pack that peaked sharply mid-month reads lower here than a single measurement taken at the right moment would.

View the data behind this chart
Underlying data
PeriodDismal Swamp (mm)
1981489
1982900
19831,117
1984945
1985700
1986757
1987504
1988427
1989885
1990454
1991554
1992324
1993942
1994385
1995778
1996765
1997871
19981,062
19991,051
2000745
2001467
2002831
2003668
2004805
2005747
20061,198
2007525
2008705
2009688
2010668
20111,150
2012487
2013511
2014392
2015341
2016850
20171,205
2018569
20191,090
2020706
2021592
2022510
20231,110
2024877
20251,072
2026258

Read against the river

Dismal Swamp and TWENTYMILE CREEK NEAR ADEL,OREG. both sit in this drainage area, and their records overlap by 10 years. That is the span the two have in common, not a count of years both actually hold — either record may have gaps inside it. The two are shown separately rather than on one axis: millimetres of stored water and cubic metres per second are not commensurable, and a difference between them would mean nothing.

Being in the same drainage area does not put the snowpack upstream of the gauge. A subbasin is an area, and snow on one tributary can join the river below a gauge on another — so a weak relationship here may say more about which tributary was measured than about the snow.

Every gauge Hydrionis holds within this area

Gauges within the Warner Lakes and what each holds
GaugeMeasuresValuesRecord
DEEP CREEK ABOVE ADEL,OREG.burned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2171923–2026
TWENTYMILE CREEK NEAR ADEL,OREG.burned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2061910–2026
HONEY CREEK NEAR PLUSH,OREG.catchment area, annual maximum river flow711910–2026
CAMAS CREEK NEAR LAKEVIEW,OREG.catchment area, annual maximum river flow271913–2026
DRAKE CREEK NEAR ADEL,OREG.catchment area, annual maximum river flow271915–2026

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 — 17120007. 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
DEEP CREEK ABOVE ADEL,OREG.Stated 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
TWENTYMILE CREEK NEAR ADEL,OREG.Stated 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
HONEY CREEK NEAR PLUSH,OREG.Stated 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
CAMAS CREEK NEAR LAKEVIEW,OREG.Stated 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
DRAKE CREEK NEAR ADEL,OREG.Stated 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 spanned117yes, 20 or more
Values held1,100yes, 1000 or more
Distinct measurements6yes, 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), Warner Lakes gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-warner-lakes/

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 Warner Lakes 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 confidence1991-05-20

Source: USGS — National Water Information System, USGS site 10371500, 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.