The monitoring network within this area

Hydrionis holds 2,618 values from 7 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.

7
Gauges
2,618
Values held
1904–2026
Record spans
Gauges within the Upper Laramie huc8 subbasin
7 monitoring points, positioned as the publisher records them.
Gauges within the Upper Laramie huc8 subbasinLARAMIE RIVER NEAR GLENDEVEY, CO, LARAMIE RIVER NEAR JELM, WY, LARAMIE RIVER AT TWO RIVERS, WY, LITTLE LARAMIE RIVER NEAR FILMORE, WY, LITTLE LARAMIE RIVER AT TWO RIVERS, WY, LARAMIE R AND PIONEER CANAL NR WOODS LANDING, WY, LARAMIE RIVER NEAR LOOKOUT, WYLARAMIE RIVER NEAR GLENDEVEY, COLARAMIE RIVER NEAR JELM, WYLARAMIE RIVER AT TWO RIVERS, WYLITTLE LARAMIE RIVER NEAR FILMORE, WYLITTLE LARAMIE RIVER AT TWO RIVERS, WYLARAMIE R AND PIONEER CANAL NR WOODS LANDING, WYLARAMIE RIVER NEAR LOOKOUT, 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 LITTLE LARAMIE RIVER NEAR FILMORE, WY
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1911–2015.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at LITTLE LARAMIE RIVER NEAR FILMORE, WYLargest measured flow of each year at LITTLE LARAMIE RIVER NEAR FILMORE, WY: LITTLE LARAMIE RIVER NEAR FILMORE, WY in m³/s, from 1911 to 2015.Hurricane Katrina water and sanitation collapse0255075100m³/s19111925194419571970198319962009

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
PeriodLITTLE LARAMIE RIVER NEAR FILMORE, WY (m³/s)
191130.6
191240.8
191468.0
191523.2
191620.9
191754.4
191854.4
191927.3
192051.0
192153.2
192229.2
192339.6
192448.7
192527.2
192655.2
193333.7
19349.40
193539.9
193630.6
193726.0
193832.3
193920.9
194018.0
194124.5
194241.6
194347.0
194418.5
194527.6
194629.7
194739.1
194832.3
194948.4
195031.7
195137.1
195235.4
195342.8
195420.7
195510.1
195628.6
195738.5
195831.7
195931.7
196022.8
196122.6
196221.7
196320.3
196425.3
196597.7
196613.5
196730.0
196825.2
196920.3
197039.4
197148.4
197246.4
197326.1
197425.3
197528.6
197618.0
197717.5
197837.9
197941.9
198035.4
198119.0
198242.8
198344.7
198429.2
198528.1
198654.9
198713.6
198832.3
198910.9
199027.0
199126.8
199215.8
199336.0
199427.1
199540.5
199628.1
199737.1
199819.9
199927.7
200021.1
200118.3
200210.1
200328.9
200411.7
200521.7
200625.9
200715.7
200823.9
200938.5
201056.9
201149.0
201211.3
201319.3
201446.7
201532.6

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 held1911–2015
Completeness93.3% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 2 separate periods inside 1911–2015 hold no value. The longest runs from 1927 to 1932 — 6 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1911 and is not continuous from it: 105 years separate the first value from the last, and 93% 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 LARAMIE RIVER NEAR GLENDEVEY, CO, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1912–1981.
Water leaving the catchment above LARAMIE RIVER NEAR GLENDEVEY, CO, as a depthWater leaving the catchment above LARAMIE RIVER NEAR GLENDEVEY, CO, as a depth: LARAMIE RIVER NEAR GLENDEVEY, CO in mm, from 1912 to 1981.0200400mm19121923193219411950195919681977LARAMIE RIVER NEAR GLENDEVEY, CO 1912: 353 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1915: 209 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1916: 256 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1917: 473 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1918: 398 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1919: 146 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1920: 330 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1921: 354 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1922: 178 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1923: 362 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1924: 310 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1925: 190 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1926: 344 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1927: 243 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1928: 300 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1929: 314 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1930: 181 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1931: 145 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1932: 240 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1933: 255 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1934: 91.0 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1935: 218 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1936: 188 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1937: 131 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1938: 291 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1939: 130 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1940: 183 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1941: 206 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1942: 211 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1943: 280 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1944: 159 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1945: 238 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1946: 229 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1947: 314 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1948: 203 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1949: 273 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1950: 200 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1951: 315 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1952: 296 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1953: 152 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1954: 106 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1955: 160 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1956: 268 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1957: 423 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1958: 252 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1959: 232 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1960: 217 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1961: 299 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1962: 327 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1963: 138 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1964: 199 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1965: 326 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1966: 129 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1967: 277 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1968: 245 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1969: 217 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1970: 343 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1971: 340 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1972: 240 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1973: 283 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1974: 280 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1975: 249 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1976: 181 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1977: 96.0 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1978: 270 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1979: 289 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1980: 252 mmLARAMIE RIVER NEAR GLENDEVEY, CO 1981: 140 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
PeriodLARAMIE RIVER NEAR GLENDEVEY, CO (mm)
1912353
1915209
1916256
1917473
1918398
1919146
1920330
1921354
1922178
1923362
1924310
1925190
1926344
1927243
1928300
1929314
1930181
1931145
1932240
1933255
193491.0
1935218
1936188
1937131
1938291
1939130
1940183
1941206
1942211
1943280
1944159
1945238
1946229
1947314
1948203
1949273
1950200
1951315
1952296
1953152
1954106
1955160
1956268
1957423
1958252
1959232
1960217
1961299
1962327
1963138
1964199
1965326
1966129
1967277
1968245
1969217
1970343
1971340
1972240
1973283
1974280
1975249
1976181
197796.0
1978270
1979289
1980252
1981140

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 held1912–1981
Completeness97.1% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • One period inside 1912–1981 holds no value: 1913 to 1914, 2 years with no reading. It is drawn as a break in the line and is never interpolated across.
ContinuityThe record begins in 1912 and is not continuous from it: 70 years separate the first value from the last, and 97% 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

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

779
Fullest snowpack recorded at Roach, in 1986 (mm of water)
184
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 Roach
Water years 1981–2026. Each point is the fullest month of that snow season.
Peak snowpack at RoachPeak snowpack at Roach: Roach in mm, from 1981 to 2026.0200400600800mm19811987199319992005201120172023Roach 1981: 258 mmRoach 1982: 469 mmRoach 1983: 686 mmRoach 1984: 554 mmRoach 1985: 413 mmRoach 1986: 779 mmRoach 1987: 279 mmRoach 1988: 456 mmRoach 1989: 343 mmRoach 1990: 443 mmRoach 1991: 401 mmRoach 1992: 315 mmRoach 1993: 515 mmRoach 1994: 369 mmRoach 1995: 468 mmRoach 1996: 578 mmRoach 1997: 623 mmRoach 1998: 400 mmRoach 1999: 435 mmRoach 2000: 363 mmRoach 2001: 353 mmRoach 2002: 219 mmRoach 2003: 452 mmRoach 2004: 356 mmRoach 2005: 357 mmRoach 2006: 399 mmRoach 2007: 457 mmRoach 2008: 532 mmRoach 2009: 454 mmRoach 2010: 497 mmRoach 2011: 665 mmRoach 2012: 317 mmRoach 2013: 369 mmRoach 2014: 555 mmRoach 2015: 279 mmRoach 2016: 483 mmRoach 2017: 401 mmRoach 2018: 350 mmRoach 2019: 431 mmRoach 2020: 397 mmRoach 2021: 381 mmRoach 2022: 412 mmRoach 2023: 461 mmRoach 2024: 356 mmRoach 2025: 313 mmRoach 2026: 184 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
PeriodRoach (mm)
1981258
1982469
1983686
1984554
1985413
1986779
1987279
1988456
1989343
1990443
1991401
1992315
1993515
1994369
1995468
1996578
1997623
1998400
1999435
2000363
2001353
2002219
2003452
2004356
2005357
2006399
2007457
2008532
2009454
2010497
2011665
2012317
2013369
2014555
2015279
2016483
2017401
2018350
2019431
2020397
2021381
2022412
2023461
2024356
2025313
2026184

Why the snow is not read against the river here

Peak snow water equivalent and Mean river flow, water year overlap for only 1 year at these subjects. A relationship read off a span that short is reading the weather of a few seasons.

Every gauge Hydrionis holds within this area

Gauges within the Upper Laramie and what each holds
GaugeMeasuresValuesRecord
LITTLE LARAMIE RIVER NEAR FILMORE, WYburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2401911–2026
LARAMIE RIVER NEAR GLENDEVEY, COburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2381904–2026
LARAMIE RIVER NEAR JELM, WYburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2181905–2026
LARAMIE RIVER AT TWO RIVERS, WYburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year1971910–2026
LITTLE LARAMIE RIVER AT TWO RIVERS, WYburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year1941911–2026
LARAMIE R AND PIONEER CANAL NR WOODS LANDING, WYcatchment area, annual maximum river flow931912–2026
LARAMIE RIVER NEAR LOOKOUT, WYcatchment area, annual maximum river flow701912–2026

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 — 10180010. 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
LITTLE LARAMIE RIVER NEAR FILMORE, 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
LARAMIE RIVER NEAR GLENDEVEY, COStated 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
LARAMIE RIVER NEAR JELM, 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
LARAMIE RIVER AT TWO RIVERS, 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
LITTLE LARAMIE RIVER AT TWO RIVERS, 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
LARAMIE R AND PIONEER CANAL NR WOODS LANDING, 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
LARAMIE RIVER NEAR LOOKOUT, 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 5 of them, which makes it a full profile.

Information-gain signals held for this water body
SignalHeldCounts
Gauges holding a real record7yes, 3 or more
Years spanned123yes, 20 or more
Values held2,618yes, 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 Laramie gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-upper-laramie/

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 Laramie 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 confidence2015-06-03

Source: USGS — National Water Information System, USGS site 06661000, 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.