The monitoring network within this area

Hydrionis holds 1,138 values from 3 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.

3
Gauges
1,138
Values held
1910–2026
Record spans
Gauges within the Saguache huc8 subbasin
3 monitoring points, positioned as the publisher records them.
Gauges within the Saguache huc8 subbasinSAGUACHE CREEK NEAR SAGUACHE, CO, CARNERO CREEK NEAR LA GARITA, CO., LA GARITA CREEK NEAR LA GARITA, COSAGUACHE CREEK NEAR SAGUACHE, COCARNERO CREEK NEAR LA GARITA, CO.LA GARITA CREEK NEAR LA GARITA, 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 SAGUACHE CREEK NEAR SAGUACHE, CO
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1911–2007.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at SAGUACHE CREEK NEAR SAGUACHE, COLargest measured flow of each year at SAGUACHE CREEK NEAR SAGUACHE, CO: SAGUACHE CREEK NEAR SAGUACHE, CO in m³/s, from 1911 to 2007.Hurricane Katrina water and sanitation collapse010203040m³/s19111923193419451956196719781997

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
PeriodSAGUACHE CREEK NEAR SAGUACHE, CO (m³/s)
191110.2
191212.7
191415.7
191513.1
19168.75
191715.0
19187.08
191916.0
192017.1
192121.1
19229.77
192313.6
192419.3
19257.33
192613.3
19279.74
192821.4
192916.7
19307.11
19316.23
193217.8
193312.2
19343.45
193512.8
19363.94
193711.0
193813.3
19397.56
19403.88
194117.0
194221.2
19434.67
194417.4
19455.15
19464.30
19478.30
194820.9
194919.7
19503.20
19516.51
195216.0
195312.8
19544.08
19553.28
19564.36
195720.7
195819.0
19593.43
19607.48
19614.39
19628.13
19635.61
196422.4
196516.8
19664.70
19673.62
196813.1
19698.95
197012.1
19716.31
19724.64
197311.4
19743.37
19759.09
19765.80
19773.68
19784.59
197910.8
19809.51
19812.38
19826.31
19915.52
19924.53
199311.2
19945.35
199514.8
19964.50
19978.30
19987.59
199934.5
20005.47
200110.9
20021.90
20034.64
20044.79
20058.18
20063.96
20077.08

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 held1911–2007
Completeness90.7% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 2 separate periods inside 1911–2007 hold no value. The longest runs from 1983 to 1990 — 8 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: 97 years separate the first value from the last, and 91% 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 SAGUACHE CREEK NEAR SAGUACHE, 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. 1911–2006.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above SAGUACHE CREEK NEAR SAGUACHE, CO, as a depthWater leaving the catchment above SAGUACHE CREEK NEAR SAGUACHE, CO, as a depth: SAGUACHE CREEK NEAR SAGUACHE, CO in mm, from 1911 to 2006.Hurricane Katrina water and sanitation collapse020406080mm19111926193819501962197419861998

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
PeriodSAGUACHE CREEK NEAR SAGUACHE, CO (mm)
191155.0
191547.0
191650.0
191753.0
191839.0
191962.0
192057.0
192164.0
192243.0
192353.0
192467.0
192541.0
192649.0
192749.0
192858.0
192958.0
193035.0
193124.0
193246.0
193329.0
193418.0
193536.0
193628.0
193734.0
193850.0
193935.0
194017.0
194159.0
194262.0
194328.0
194450.0
194535.0
194627.0
194743.0
194854.0
194959.0
195020.0
195118.0
195243.0
195333.0
195421.0
195519.0
195619.0
195769.0
195851.0
195925.0
196034.0
196125.0
196237.0
196317.0
196425.0
196561.0
196627.0
196722.0
196847.0
196934.0
197056.0
197129.0
197227.0
197344.0
197421.0
197540.0
197631.0
197716.0
197821.0
197945.0
198037.0
198118.0
198242.0
198350.0
198459.0
198556.0
198648.0
198765.0
198828.0
198926.0
199031.0
199130.0
199229.0
199339.0
199426.0
199548.0
199624.0
199739.0
199840.0
199947.0
200027.0
200140.0
200213.0
200319.0
200428.0
200531.0
200626.0

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 held1911–2006
Completeness96.9% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • One period inside 1911–2006 holds no value: 1912 to 1914, 3 years with no reading. It is drawn as a break in the line and is never interpolated across.
ContinuityThe record begins in 1911 and is not continuous from it: 96 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.

199
Fullest snowpack recorded at Cochetopa Pass, in 2019 (mm of water)
59
Thinnest, in 2018 (mm of water)
March
Month the pack is usually at its fullest
May
Month the pack has gone by, in half of years
Peak snowpack at Cochetopa Pass
Water years 2005–2026. Each point is the fullest month of that snow season.
Peak snowpack at Cochetopa PassPeak snowpack at Cochetopa Pass: Cochetopa Pass in mm, from 2005 to 2026.050100150200mm20052008201120142017202020232026Cochetopa Pass 2005: 113 mmCochetopa Pass 2006: 88.0 mmCochetopa Pass 2007: 84.0 mmCochetopa Pass 2008: 148 mmCochetopa Pass 2009: 73.0 mmCochetopa Pass 2010: 100 mmCochetopa Pass 2011: 99.0 mmCochetopa Pass 2012: 69.0 mmCochetopa Pass 2013: 70.0 mmCochetopa Pass 2014: 124 mmCochetopa Pass 2015: 115 mmCochetopa Pass 2016: 122 mmCochetopa Pass 2017: 107 mmCochetopa Pass 2018: 59.0 mmCochetopa Pass 2019: 199 mmCochetopa Pass 2020: 150 mmCochetopa Pass 2021: 137 mmCochetopa Pass 2022: 91.0 mmCochetopa Pass 2023: 125 mmCochetopa Pass 2024: 131 mmCochetopa Pass 2025: 120 mmCochetopa Pass 2026: 82.0 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
PeriodCochetopa Pass (mm)
2005113
200688.0
200784.0
2008148
200973.0
2010100
201199.0
201269.0
201370.0
2014124
2015115
2016122
2017107
201859.0
2019199
2020150
2021137
202291.0
2023125
2024131
2025120
202682.0

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 Saguache and what each holds
GaugeMeasuresValuesRecord
SAGUACHE CREEK NEAR SAGUACHE, COburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3111910–2026
LA GARITA CREEK NEAR LA GARITA, COcatchment area, annual maximum river flow711920–2026
CARNERO CREEK NEAR LA GARITA, CO.catchment area, annual maximum river flow591920–2026

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 — 13010004. 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
SAGUACHE CREEK NEAR SAGUACHE, 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
LA GARITA CREEK NEAR LA GARITA, 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
CARNERO CREEK NEAR LA GARITA, 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 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 held1,138yes, 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), Saguache gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-saguache/

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 Saguache 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 confidence2007-06-04

Source: USGS — National Water Information System, USGS site 08227000, 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.