The monitoring network within this area

Hydrionis holds 2,430 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
2,430
Values held
1882–2026
Record spans
Gauges within the Cache La Poudre huc8 subbasin
2 monitoring points, positioned as the publisher records them.
Gauges within the Cache La Poudre huc8 subbasinCACHE LA POUDRE RIV AT MO OF CN, NR FT COLLINS, CO, CACHE LA POUDRE RIVER NEAR GREELEY, CO.CACHE LA POUDRE RIV AT MO OF CN, NR FT COLLINS, COCACHE LA POUDRE RIVER NEAR GREELEY, CO.

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 CACHE LA POUDRE RIV AT MO OF CN, NR FT COLLINS, CO
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1882–2007.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at CACHE LA POUDRE RIV AT MO OF CN, NR FT COLLINS, COLargest measured flow of each year at CACHE LA POUDRE RIV AT MO OF CN, NR FT COLLINS, CO: CACHE LA POUDRE RIV AT MO OF CN, NR FT COLLINS, CO in m³/s, from 1882 to 2007.Hurricane Katrina water and sanitation collapse0200400600m³/s18821898191419301946196219781994

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
PeriodCACHE LA POUDRE RIV AT MO OF CN, NR FT COLLINS, CO (m³/s)
188249.0
1883224
1884194
1885114
1886136
188785.0
188851.0
188959.5
189053.8
1891595
189290.6
189390.6
1894113
1895113
189670.8
189793.4
189853.8
1899119
1900142
1901340
190270.8
1903116
19040
1905133
190685.0
1907113
190876.5
1909167
191063.4
191169.9
1912108
191376.5
1914152
191576.5
191666.3
1917198
1918147
191947.3
1920128
1921148
1922126
1923242
1924211
192550.4
1926123
192768.2
1928115
192997.1
1930289
193164.6
193290.6
193399.1
193447.0
1935116
193692.9
193757.2
1938175
193973.1
194099.4
194161.7
194293.4
194395.7
194478.4
194559.7
194682.1
1947132
194880.7
1949172
195082.4
1951131
1952104
195370.5
195434.5
195552.1
195686.1
1957124
1958107
195975.9
196073.1
196183.8
196269.1
196341.1
196454.9
1965136
196633.4
196762.6
196874.5
196967.7
197086.4
1971110
197296.3
1973107
197483.3
197571.1
1976208
197749.3
1978106
197993.2
1980109
198168.5
198289.8
1983187
1984113
198599.7
1986111
198747.3
198877.6
198944.5
199071.4
1991128
199248.7
199377.3
199452.4
1995134
199680.1
199793.7
199853.2
1999165
200050.7
200149.3
200224.9
2003107
200445.3
200564.3
200651.0
200756.9

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 held1882–2007
Completeness100.0% of the periods in that span are held.
ContinuityContinuous: every year from 1882 to 2007 is held.
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 CACHE LA POUDRE RIV AT MO OF CN, NR FT COLLINS, 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. 1885–2006.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above CACHE LA POUDRE RIV AT MO OF CN, NR FT COLLINS, CO, as a depthWater leaving the catchment above CACHE LA POUDRE RIV AT MO OF CN, NR FT COLLINS, CO, as a depth: CACHE LA POUDRE RIV AT MO OF CN, NR FT COLLINS, CO in mm, from 1885 to 2006.Hurricane Katrina water and sanitation collapse0100200300mm18851900191919341949196419791994

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
PeriodCACHE LA POUDRE RIV AT MO OF CN, NR FT COLLINS, CO (mm)
1885222
1886140
1887140
188882.0
188992.0
1890110
1891129
189296.0
1893104
1894148
1895171
1896106
1897158
189888.0
1899185
1900223
1901155
190286.0
1905162
1906135
1907176
1908120
1911113
1912145
1913103
1914179
1915111
1916124
1917233
1918142
191973.0
1920165
1921179
192292.0
1923206
1924200
1925103
1926167
1927119
1928136
1929147
1930102
193176.0
1932116
1933125
193460.0
1935129
1936133
1937102
1938160
193995.0
194077.0
1941101
1942148
1943151
1944101
1945120
194698.0
1947143
1948100
1949154
195095.0
1951136
1952122
195374.0
195445.0
195565.0
195696.0
1957148
1958107
195998.0
196091.0
1961131
1962115
196350.0
196471.0
1965128
196644.0
196776.0
196897.0
196987.0
1970120
1971140
197280.0
1973148
1974119
197599.0
197671.0
197742.0
1978122
1979133
1980194
198159.0
1982116
1983297
1984174
198588.0
1986143
198760.0
198888.0
198958.0
199097.0
199193.0
199280.0
1993106
199468.0
1995142
1996121
1997137
1998110
1999152
200068.0
200163.0
200228.0
2003100
200474.0
200594.0
200667.0

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 held1885–2006
Completeness96.7% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 2 separate periods inside 1885–2006 hold no value. The longest runs from 1903 to 1904 — 2 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1885 and is not continuous from it: 122 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

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

794
Fullest snowpack recorded at Deadman Hill, in 2011 (mm of water)
240
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 Deadman Hill
Water years 1979–2026. Each point is the fullest month of that snow season.
Peak snowpack at Deadman HillPeak snowpack at Deadman Hill: Deadman Hill in mm, from 1979 to 2026.0200400600800mm19791985199119972003200920152021Deadman Hill 1979: 513 mmDeadman Hill 1980: 533 mmDeadman Hill 1981: 330 mmDeadman Hill 1982: 546 mmDeadman Hill 1983: 648 mmDeadman Hill 1984: 543 mmDeadman Hill 1985: 420 mmDeadman Hill 1986: 693 mmDeadman Hill 1987: 310 mmDeadman Hill 1988: 504 mmDeadman Hill 1989: 448 mmDeadman Hill 1990: 423 mmDeadman Hill 1991: 420 mmDeadman Hill 1992: 406 mmDeadman Hill 1993: 502 mmDeadman Hill 1994: 474 mmDeadman Hill 1995: 602 mmDeadman Hill 1996: 622 mmDeadman Hill 1997: 487 mmDeadman Hill 1998: 408 mmDeadman Hill 1999: 495 mmDeadman Hill 2000: 412 mmDeadman Hill 2001: 353 mmDeadman Hill 2002: 265 mmDeadman Hill 2003: 457 mmDeadman Hill 2004: 356 mmDeadman Hill 2005: 411 mmDeadman Hill 2006: 417 mmDeadman Hill 2007: 367 mmDeadman Hill 2008: 518 mmDeadman Hill 2009: 496 mmDeadman Hill 2010: 550 mmDeadman Hill 2011: 794 mmDeadman Hill 2012: 407 mmDeadman Hill 2013: 403 mmDeadman Hill 2014: 661 mmDeadman Hill 2015: 437 mmDeadman Hill 2016: 553 mmDeadman Hill 2017: 530 mmDeadman Hill 2018: 555 mmDeadman Hill 2019: 555 mmDeadman Hill 2020: 514 mmDeadman Hill 2021: 507 mmDeadman Hill 2022: 504 mmDeadman Hill 2023: 514 mmDeadman Hill 2024: 524 mmDeadman Hill 2025: 441 mmDeadman Hill 2026: 240 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
PeriodDeadman Hill (mm)
1979513
1980533
1981330
1982546
1983648
1984543
1985420
1986693
1987310
1988504
1989448
1990423
1991420
1992406
1993502
1994474
1995602
1996622
1997487
1998408
1999495
2000412
2001353
2002265
2003457
2004356
2005411
2006417
2007367
2008518
2009496
2010550
2011794
2012407
2013403
2014661
2015437
2016553
2017530
2018555
2019555
2020514
2021507
2022504
2023514
2024524
2025441
2026240

Read against the river

Deadman Hill and CACHE LA POUDRE RIV AT MO OF CN, NR FT COLLINS, CO both sit in this drainage area, and their records overlap by 27 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 Cache La Poudre and what each holds
GaugeMeasuresValuesRecord
CACHE LA POUDRE RIV AT MO OF CN, NR FT COLLINS, COburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3991882–2026
CACHE LA POUDRE RIVER NEAR GREELEY, CO.burned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2711903–2026

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 — 10190007. 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
CACHE LA POUDRE RIV AT MO OF CN, NR FT COLLINS, 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
CACHE LA POUDRE RIVER NEAR GREELEY, CO.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 4 of them, which makes it a full profile.

Information-gain signals held for this water body
SignalHeldCounts
Gauges holding a real record2no
Years spanned145yes, 20 or more
Values held2,430yes, 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), Cache La Poudre gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-cache-la-poudre/

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 Cache La Poudre 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 confidence2007-06-16

Source: USGS — National Water Information System, USGS site 06752000, 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.