The monitoring network within this area

Hydrionis holds 3,867 values from 10 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.

10
Gauges
3,867
Values held
1899–2026
Record spans
Gauges within the Alamosa-Trinchera huc8 subbasin
10 monitoring points, positioned as the publisher records them.
Gauges within the Alamosa-Trinchera huc8 subbasinALAMOSA RIVER ABOVE TERRACE RESERVOIR, CO., UTE CREEK NEAR FORT GARLAND, CO, CULEBRA CREEK AT SAN LUIS, CO, RIO GRANDE NEAR LOBATOS, CO, RIO GRANDE NEAR MONTE VISTA, CO., RIO GRANDE AT ALAMOSA, CO., PINOS CREEK NEAR DEL NORTE, CO., TRINCHERA C AB TURNERS RANCH, NR FT GARLAND, CO., SANGRE DE CRISTO CREEK NEAR FORT GARLAND, CO., TRINCHERA CREEK BELOW SMITH RES, NR BLANCA, CO.ALAMOSA RIVER ABOVE TERRACE RESERVOIR, CO.UTE CREEK NEAR FORT GARLAND, COCULEBRA CREEK AT SAN LUIS, CORIO GRANDE NEAR LOBATOS, CORIO GRANDE NEAR MONTE VISTA, CO.RIO GRANDE AT ALAMOSA, CO.PINOS CREEK NEAR DEL NORTE, CO.TRINCHERA C AB TURNERS RANCH, NR FT GARLAND, CO.SANGRE DE CRISTO CREEK NEAR FORT GARLAND, CO.TRINCHERA CREEK BELOW SMITH RES, NR BLANCA, 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 RIO GRANDE NEAR LOBATOS, CO
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1900–2024.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at RIO GRANDE NEAR LOBATOS, COLargest measured flow of each year at RIO GRANDE NEAR LOBATOS, CO: RIO GRANDE NEAR LOBATOS, CO in m³/s, from 1900 to 2024.Hurricane Katrina water and sanitation collapse0100200300400m³/s19001915193219481967198420012017

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
PeriodRIO GRANDE NEAR LOBATOS, CO (m³/s)
1900133
1901103
190216.0
1903362
190421.3
1905374
1906237
1907249
190865.1
1909216
1910152
1911167
1912248
191362.3
1914130
1915115
1916170
1917222
191847.3
1919144
1920264
1921357
1922207
1923117
1924217
192533.4
192694.3
1927278
1929101
193045.0
1932164
193364.8
193418.8
1935130
193671.9
1937124
1938114
193946.4
194033.7
1941229
1942158
194339.6
1944182
194581.6
194755.5
1948244
1949264
1950193
1952328
195328.2
195619.3
1957108
1958121
195911.8
196057.8
196140.8
196274.2
196312.0
1965107
196637.7
196731.4
196869.9
196977.3
197054.7
197148.7
197224.2
1973101
197422.2
197570.5
197641.1
197827.7
1979137
198091.5
198255.2
198391.5
198496.0
1985177
1986175
1987191
198824.0
198953.0
199052.7
199160.3
199248.1
1993110
199465.7
1995179
199618.4
1997102
199965.4
200161.4
200212.5
20038.55
200440.2
2005116
200744.2
200883.3
200970.8
201046.4
201128.0
201237.1
201317.4
201430.9
201539.4
201644.7
201770.2
201817.4
201998.5
202016.1
202127.0
202230.6
2023104
202422.1

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 held1900–2024
Completeness90.4% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 11 separate periods inside 1900–2024 hold no value. The longest runs from 1954 to 1955 — 2 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1900 and is not continuous from it: 125 years separate the first value from the last, and 90% 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 RIO GRANDE NEAR LOBATOS, 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. 1900–2023.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above RIO GRANDE NEAR LOBATOS, CO, as a depthWater leaving the catchment above RIO GRANDE NEAR LOBATOS, CO, as a depth: RIO GRANDE NEAR LOBATOS, CO in mm, from 1900 to 2023.Hurricane Katrina water and sanitation collapse050100150mm19001916193219481964198019962012

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
PeriodRIO GRANDE NEAR LOBATOS, CO (mm)
190030.0
190128.0
190210.0
190363.0
190419.0
190599.0
190685.0
1907144
190836.0
190993.0
191056.0
1911104
191285.0
191329.0
191459.0
191547.0
191677.0
191780.0
191826.0
191961.0
1920104
192186.0
192267.0
192369.0
192475.0
192532.0
192643.0
192772.0
192832.0
192960.0
193027.0
193113.0
193260.0
193324.0
193410.0
193536.0
193628.0
193747.0
193857.0
193921.0
194011.0
194195.0
194268.0
194318.0
194461.0
194528.0
194612.0
194723.0
194866.0
194957.0
195013.0
19517.00
195247.0
195312.0
19546.00
19556.00
19567.00
195745.0
195836.0
19599.00
196020.0
196117.0
196232.0
19637.00
19646.00
196550.0
196626.0
196716.0
196833.0
196942.0
197032.0
197121.0
197216.0
197352.0
197412.0
197547.0
197625.0
19776.00
197817.0
197963.0
198045.0
198113.0
198244.0
198339.0
198442.0
198588.0
198680.0
198783.0
198818.0
198922.0
199018.0
199131.0
199224.0
199340.0
199429.0
199553.0
199613.0
199756.0
199824.0
199946.0
200011.0
200129.0
20027.00
20037.00
200422.0
200545.0
200623.0
200729.0
200839.0
200929.0
201023.0
201120.0
201213.0
201313.0
201423.0
201525.0
201628.0
201741.0
20189.00
201956.0
202011.0
202116.0
202219.0
202340.0

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 held1900–2023
Completeness100.0% of the periods in that span are held.
ContinuityContinuous: every year from 1900 to 2023 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

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

530
Fullest snowpack recorded at Culebra #2, in 1983 (mm of water)
137
Thinnest, in 2026 (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 Culebra #2
Water years 1980–2026. Each point is the fullest month of that snow season.
Peak snowpack at Culebra #2Peak snowpack at Culebra #2: Culebra #2 in mm, from 1980 to 2026.0200400600mm19801986199219982004201020162022Culebra #2 1980: 431 mmCulebra #2 1981: 169 mmCulebra #2 1982: 292 mmCulebra #2 1983: 530 mmCulebra #2 1984: 404 mmCulebra #2 1985: 412 mmCulebra #2 1986: 192 mmCulebra #2 1987: 319 mmCulebra #2 1988: 248 mmCulebra #2 1989: 361 mmCulebra #2 1990: 309 mmCulebra #2 1991: 349 mmCulebra #2 1992: 394 mmCulebra #2 1993: 503 mmCulebra #2 1994: 372 mmCulebra #2 1995: 422 mmCulebra #2 1996: 230 mmCulebra #2 1997: 294 mmCulebra #2 1998: 363 mmCulebra #2 1999: 176 mmCulebra #2 2000: 262 mmCulebra #2 2001: 311 mmCulebra #2 2002: 200 mmCulebra #2 2003: 318 mmCulebra #2 2004: 249 mmCulebra #2 2005: 490 mmCulebra #2 2006: 157 mmCulebra #2 2007: 324 mmCulebra #2 2008: 382 mmCulebra #2 2009: 334 mmCulebra #2 2010: 357 mmCulebra #2 2011: 205 mmCulebra #2 2012: 247 mmCulebra #2 2013: 256 mmCulebra #2 2014: 268 mmCulebra #2 2015: 321 mmCulebra #2 2016: 289 mmCulebra #2 2017: 433 mmCulebra #2 2018: 196 mmCulebra #2 2019: 397 mmCulebra #2 2020: 367 mmCulebra #2 2021: 418 mmCulebra #2 2022: 206 mmCulebra #2 2023: 306 mmCulebra #2 2024: 276 mmCulebra #2 2025: 222 mmCulebra #2 2026: 137 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
PeriodCulebra #2 (mm)
1980431
1981169
1982292
1983530
1984404
1985412
1986192
1987319
1988248
1989361
1990309
1991349
1992394
1993503
1994372
1995422
1996230
1997294
1998363
1999176
2000262
2001311
2002200
2003318
2004249
2005490
2006157
2007324
2008382
2009334
2010357
2011205
2012247
2013256
2014268
2015321
2016289
2017433
2018196
2019397
2020367
2021418
2022206
2023306
2024276
2025222
2026137

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 Alamosa-Trinchera and what each holds
GaugeMeasuresValuesRecord
RIO GRANDE NEAR LOBATOS, COburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year4041899–2026
RIO GRANDE AT ALAMOSA, CO.burned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2501912–2026
UTE CREEK NEAR FORT GARLAND, COburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2351916–2026
CULEBRA CREEK AT SAN LUIS, COburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2261927–2026
RIO GRANDE NEAR MONTE VISTA, CO.burned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year1981926–2026
ALAMOSA RIVER ABOVE TERRACE RESERVOIR, CO.burned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year1961911–2026
TRINCHERA C AB TURNERS RANCH, NR FT GARLAND, CO.catchment area, annual maximum river flow601923–2026
SANGRE DE CRISTO CREEK NEAR FORT GARLAND, CO.catchment area, annual maximum river flow581923–2026
TRINCHERA CREEK BELOW SMITH RES, NR BLANCA, CO.catchment area, annual maximum river flow521929–2026
PINOS CREEK NEAR DEL NORTE, CO.catchment area, annual maximum river flow501920–2026

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 — 13010002. 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
RIO GRANDE NEAR LOBATOS, 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
RIO GRANDE AT ALAMOSA, 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
UTE CREEK NEAR FORT GARLAND, 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
CULEBRA CREEK AT SAN LUIS, 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
RIO GRANDE NEAR MONTE VISTA, 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
ALAMOSA RIVER ABOVE TERRACE RESERVOIR, 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
TRINCHERA C AB TURNERS RANCH, NR FT GARLAND, 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
SANGRE DE CRISTO CREEK NEAR FORT GARLAND, 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
TRINCHERA CREEK BELOW SMITH RES, NR BLANCA, 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
PINOS CREEK NEAR DEL NORTE, 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 record10yes, 3 or more
Years spanned128yes, 20 or more
Values held3,867yes, 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), Alamosa-Trinchera gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-alamosa-trinchera/

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 Alamosa-Trinchera 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 confidence2024-05-12

Source: USGS — National Water Information System, USGS site 08251500, 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.