The monitoring network within this area

Hydrionis holds 3,174 values from 4 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.

4
Gauges
3,174
Values held
1906–2026
Record spans
Gauges within the Upper Wind huc8 subbasin
4 monitoring points, positioned as the publisher records them.
Gauges within the Upper Wind huc8 subbasinBull Lake Creek near Lenore, WY, WIND RIVER AT RIVERTON, WY, DRY CREEK NEAR BURRIS, WY, WILLOW CREEK NEAR CROWHEART, WYBull Lake Creek near Lenore, WYWIND RIVER AT RIVERTON, WYDRY CREEK NEAR BURRIS, WYWILLOW CREEK NEAR CROWHEART, WY

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 WIND RIVER AT RIVERTON, WY
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1906–2024.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at WIND RIVER AT RIVERTON, WYLargest measured flow of each year at WIND RIVER AT RIVERTON, WY: WIND RIVER AT RIVERTON, WY in m³/s, from 1906 to 2024.Hurricane Katrina water and sanitation collapse0100200300400m³/s19061924193919541969198419992014

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
PeriodWIND RIVER AT RIVERTON, WY (m³/s)
1906348
1908249
1911314
1912255
1913309
1914249
1915156
1916219
1917270
1918263
191964.6
1920249
1921345
1922208
1923323
1924237
1925252
1926129
1927266
1928309
1929134
1930255
1931220
1932249
1933269
1934156
1935377
1936163
1937183
1938111
1939121
1940120
1941155
1942187
1943187
1944206
1945172
1946112
1947238
1948171
1949138
1950135
1951217
1952163
1953218
1954156
195577.0
1956232
1957270
1958191
1959117
196056.1
1961124
1962189
1963256
1964164
1965212
196674.2
1967270
1968127
1969113
1970133
1971266
1972217
1973151
1974223
1975212
1976122
197750.7
1978156
1979127
1980158
1981220
1982164
1983199
1984114
198560.3
1986207
198776.2
198860.3
1989112
199070.2
1991240
199281.3
199393.7
199467.7
1995216
1996180
1997286
1998174
1999255
200062.3
200126.2
200274.8
2003123
200478.7
2005176
200658.3
200749.6
2008105
2009174
2010180
2011317
201283.5
201360.6
2014180
2015221
2016149
2017334
2018275
2019178
2020181
2021121
2022245
2023272
2024120

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 held1906–2024
Completeness97.5% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 2 separate periods inside 1906–2024 hold no value. The longest runs from 1909 to 1910 — 2 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1906 and is not continuous from it: 119 years separate the first value from the last, and 97% 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 WIND RIVER AT RIVERTON, WY, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1913–2024.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above WIND RIVER AT RIVERTON, WY, as a depthWater leaving the catchment above WIND RIVER AT RIVERTON, WY, as a depth: WIND RIVER AT RIVERTON, WY in mm, from 1913 to 2024.Hurricane Katrina water and sanitation collapse0100200mm19131932194619601974198820022016

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
PeriodWIND RIVER AT RIVERTON, WY (mm)
1913241
1915163
1916196
191987.0
1920203
1921200
1922191
1923225
1924188
1925211
1926146
1927229
1930185
1931126
1932149
1933141
193478.0
1935138
1936144
1937127
1938122
193980.0
194065.0
1941134
1942135
1943190
1944148
1945143
1946108
1947190
1948133
1949125
1950147
1951189
1952106
195381.0
195492.0
195548.0
1956146
1957171
195893.0
195969.0
196036.0
196162.0
1962120
1963108
196494.0
1965170
196652.0
1967165
196894.0
196975.0
197062.0
1971173
1972142
197388.0
1974119
1975114
1976101
197733.0
1978110
197967.0
198092.0
198154.0
1982116
1983130
198486.0
198546.0
1986119
198755.0
198828.0
198959.0
199053.0
1991112
199238.0
199368.0
199431.0
1995121
1996101
1997146
1998110
1999138
200034.0
200123.0
200236.0
200346.0
200437.0
200569.0
200636.0
200724.0
200862.0
2009115
201078.0
2011138
201242.0
201350.0
2014128
2015105
201683.0
2017206
2018155
201994.0
202072.0
202154.0
202274.0
2023137
202449.0

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 held1913–2024
Completeness95.5% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 3 separate periods inside 1913–2024 hold no value. The longest runs from 1917 to 1918 — 2 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1913 and is not continuous from it: 112 years separate the first value from the last, and 96% 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

The snow standing above this water

5 automated snow stations sit inside this drainage area, weighing the snowpack rather than measuring how deep it is.

480
Fullest snowpack recorded at Little Warm, in 2017 (mm of water)
175
Thinnest, in 2004 (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 Little Warm
Water years 1979–2026. Each point is the fullest month of that snow season.
Peak snowpack at Little WarmPeak snowpack at Little Warm: Little Warm in mm, from 1979 to 2026.0200400mm19791985199119972003200920152021Little Warm 1979: 238 mmLittle Warm 1980: 275 mmLittle Warm 1981: 206 mmLittle Warm 1982: 382 mmLittle Warm 1983: 307 mmLittle Warm 1984: 299 mmLittle Warm 1985: 231 mmLittle Warm 1986: 424 mmLittle Warm 1987: 255 mmLittle Warm 1988: 211 mmLittle Warm 1989: 306 mmLittle Warm 1990: 226 mmLittle Warm 1991: 303 mmLittle Warm 1992: 180 mmLittle Warm 1993: 267 mmLittle Warm 1994: 199 mmLittle Warm 1995: 367 mmLittle Warm 1996: 411 mmLittle Warm 1997: 473 mmLittle Warm 1998: 305 mmLittle Warm 1999: 409 mmLittle Warm 2000: 250 mmLittle Warm 2001: 204 mmLittle Warm 2002: 244 mmLittle Warm 2003: 232 mmLittle Warm 2004: 175 mmLittle Warm 2005: 199 mmLittle Warm 2006: 213 mmLittle Warm 2007: 207 mmLittle Warm 2008: 271 mmLittle Warm 2009: 319 mmLittle Warm 2010: 211 mmLittle Warm 2011: 414 mmLittle Warm 2012: 208 mmLittle Warm 2013: 245 mmLittle Warm 2014: 363 mmLittle Warm 2015: 224 mmLittle Warm 2016: 215 mmLittle Warm 2017: 480 mmLittle Warm 2018: 429 mmLittle Warm 2019: 242 mmLittle Warm 2020: 325 mmLittle Warm 2021: 236 mmLittle Warm 2022: 277 mmLittle Warm 2023: 285 mmLittle Warm 2024: 246 mmLittle Warm 2025: 252 mmLittle Warm 2026: 230 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
PeriodLittle Warm (mm)
1979238
1980275
1981206
1982382
1983307
1984299
1985231
1986424
1987255
1988211
1989306
1990226
1991303
1992180
1993267
1994199
1995367
1996411
1997473
1998305
1999409
2000250
2001204
2002244
2003232
2004175
2005199
2006213
2007207
2008271
2009319
2010211
2011414
2012208
2013245
2014363
2015224
2016215
2017480
2018429
2019242
2020325
2021236
2022277
2023285
2024246
2025252
2026230

Read against the river

Little Warm and Bull Lake Creek near Lenore, WY both sit in this drainage area, and their records overlap by 38 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 Upper Wind and what each holds
GaugeMeasuresValuesRecord
WIND RIVER AT RIVERTON, WYburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3671906–2026
Bull Lake Creek near Lenore, WYburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3271918–2026
WILLOW CREEK NEAR CROWHEART, WYcatchment area, annual maximum river flow391909–2026
DRY CREEK NEAR BURRIS, WYcatchment area, annual maximum river flow371921–2026

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 — 10080001. 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
WIND RIVER AT RIVERTON, WYStated 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
Bull Lake Creek near Lenore, WYStated 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
WILLOW CREEK NEAR CROWHEART, WYStated 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
DRY CREEK NEAR BURRIS, WYStated 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 record2no
Years spanned121yes, 20 or more
Values held3,174yes, 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), Upper Wind gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-upper-wind/

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 Upper Wind 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 confidence2024-06-08

Source: USGS — National Water Information System, USGS site 06228000, 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.