The monitoring network within this area

Hydrionis holds 1,718 values from 5 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.

5
Gauges
1,718
Values held
1903–2026
Record spans
Gauges within the Pecos Headwaters huc8 subbasin
5 monitoring points, positioned as the publisher records them.
Gauges within the Pecos Headwaters huc8 subbasinPECOS RIVER NEAR PECOS, NM, PECOS RIVER NEAR ANTON CHICO, NM, GALLINAS CREEK NEAR MONTEZUMA, NM, GALLINAS CREEK AT MONTEZUMA, NM, PECOS RIVER AT SANTA ROSA, NMPECOS RIVER NEAR PECOS, NMPECOS RIVER NEAR ANTON CHICO, NMGALLINAS CREEK NEAR MONTEZUMA, NMGALLINAS CREEK AT MONTEZUMA, NMPECOS RIVER AT SANTA ROSA, NM

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 GALLINAS CREEK NEAR MONTEZUMA, NM
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1915–2024.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at GALLINAS CREEK NEAR MONTEZUMA, NMLargest measured flow of each year at GALLINAS CREEK NEAR MONTEZUMA, NM: GALLINAS CREEK NEAR MONTEZUMA, NM in m³/s, from 1915 to 2024.Hurricane Katrina water and sanitation collapse0100200m³/s19151930194419591973198620012014

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
PeriodGALLINAS CREEK NEAR MONTEZUMA, NM (m³/s)
191537.1
191648.7
19174.25
1918106
191987.8
192024.9
1921109
192214.2
192537.1
19269.88
192774.2
19285.92
192947.3
193017.4
19326.60
19337.19
19342.86
193545.6
193632.3
19375.13
193811.0
193910.6
194058.9
1941107
1942129
194310.7
19443.71
194514.7
194615.0
194813.3
194921.8
195026.9
195154.4
195228.9
195313.0
19541.90
195513.7
19563.34
1957153
19594.98
19608.30
196139.1
19627.14
196313.0
196479.0
196514.5
1966202
196731.1
19683.26
196911.4
197124.4
197258.9
197323.6
197424.6
19753.23
19769.12
197714.0
19783.23
197960.9
198018.0
198143.3
19824.11
19833.51
198415.7
19856.99
19864.33
19876.80
198816.1
19895.55
19908.78
199182.1
19925.44
19932.94
199444.7
1996106
199728.3
19988.01
20002.18
200114.6
20024.33
20030.963
200421.0
20057.53
20069.91
20072.32
200820.6
20095.24
201043.6
20111.05
20121.81
2013102
201421.0
20156.26
20162.86
201715.9
20195.49
20201.28
20212.65
202266.0
20239.85
202473.9

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 held1915–2024
Completeness91.8% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 8 separate periods inside 1915–2024 hold no value. The longest runs from 1923 to 1924 — 2 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1915 and is not continuous from it: 110 years separate the first value from the last, and 92% 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 GALLINAS CREEK NEAR MONTEZUMA, NM, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1927–2024.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above GALLINAS CREEK NEAR MONTEZUMA, NM, as a depthWater leaving the catchment above GALLINAS CREEK NEAR MONTEZUMA, NM, as a depth: GALLINAS CREEK NEAR MONTEZUMA, NM in mm, from 1927 to 2024.Hurricane Katrina water and sanitation collapse0100200300400mm19271940195319661979199220052018

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
PeriodGALLINAS CREEK NEAR MONTEZUMA, NM (mm)
192767.0
192879.0
1929132
193072.0
1931145
193289.0
193337.0
193413.0
193581.0
193636.0
193770.0
193850.0
193969.0
194051.0
1941387
1942173
194335.0
194462.0
194567.0
194660.0
194735.0
194860.0
1949104
195054.0
195124.0
195256.0
195315.0
195412.0
195555.0
19567.00
1957120
1958193
195952.0
1960105
1961158
196258.0
196337.0
196426.0
196559.0
196659.0
196754.0
196864.0
196989.0
197054.0
197138.0
197288.0
1973204
197425.0
197572.0
197627.0
197727.0
197835.0
1979154
198053.0
198149.0
198254.0
198397.0
198453.0
1985151
198670.0
1987146
198891.0
198950.0
199087.0
1991246
199290.0
199381.0
1994138
199589.0
199667.0
1997200
1998126
199988.0
200034.0
200168.0
200218.0
200325.0
2004109
2005154
200669.0
200766.0
200891.0
200952.0
2010110
201119.0
201237.0
201380.0
201439.0
201595.0
201680.0
201772.0
201824.0
201989.0
202029.0
202137.0
202297.0
202384.0
2024163

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 held1927–2024
Completeness100.0% of the periods in that span are held.
ContinuityContinuous: every year from 1927 to 2024 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

1 automated snow station sits inside this drainage area, weighing the snowpack rather than measuring how deep it is.

585
Fullest snowpack recorded at Wesner Springs, in 1993 (mm of water)
25
Thinnest, in 2006 (mm of water)
March
Month the pack is usually at its fullest
June
Month the pack has gone by, in half of years
Peak snowpack at Wesner Springs
Water years 1990–2026. Each point is the fullest month of that snow season.
Peak snowpack at Wesner SpringsPeak snowpack at Wesner Springs: Wesner Springs in mm, from 1990 to 2026.0200400600mm19901995200020052010201520202025Wesner Springs 1990: 339 mmWesner Springs 1991: 366 mmWesner Springs 1992: 471 mmWesner Springs 1993: 585 mmWesner Springs 1994: 473 mmWesner Springs 1995: 518 mmWesner Springs 1996: 216 mmWesner Springs 1997: 512 mmWesner Springs 1998: 468 mmWesner Springs 1999: 194 mmWesner Springs 2000: 177 mmWesner Springs 2001: 459 mmWesner Springs 2002: 221 mmWesner Springs 2003: 363 mmWesner Springs 2004: 398 mmWesner Springs 2005: 501 mmWesner Springs 2006: 25.0 mmWesner Springs 2007: 315 mmWesner Springs 2008: 431 mmWesner Springs 2009: 267 mmWesner Springs 2010: 381 mmWesner Springs 2011: 158 mmWesner Springs 2012: 324 mmWesner Springs 2013: 181 mmWesner Springs 2014: 198 mmWesner Springs 2015: 289 mmWesner Springs 2016: 370 mmWesner Springs 2017: 262 mmWesner Springs 2018: 25.0 mmWesner Springs 2019: 429 mmWesner Springs 2020: 348 mmWesner Springs 2021: 182 mmWesner Springs 2022: 214 mmWesner Springs 2023: 392 mmWesner Springs 2024: 317 mmWesner Springs 2025: 121 mmWesner Springs 2026: 46.0 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
PeriodWesner Springs (mm)
1990339
1991366
1992471
1993585
1994473
1995518
1996216
1997512
1998468
1999194
2000177
2001459
2002221
2003363
2004398
2005501
200625.0
2007315
2008431
2009267
2010381
2011158
2012324
2013181
2014198
2015289
2016370
2017262
201825.0
2019429
2020348
2021182
2022214
2023392
2024317
2025121
202646.0

Read against the river

Wesner Springs and PECOS RIVER NEAR PECOS, NM both sit in this drainage area, and their records overlap by 35 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 Pecos Headwaters and what each holds
GaugeMeasuresValuesRecord
GALLINAS CREEK NEAR MONTEZUMA, NMburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3411915–2026
PECOS RIVER NEAR ANTON CHICO, NMburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3331904–2026
PECOS RIVER NEAR PECOS, NMburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3311920–2026
GALLINAS CREEK AT MONTEZUMA, NMburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2041904–2026
PECOS RIVER AT SANTA ROSA, NMcatchment area, annual maximum river flow661903–2026

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 — 13060001. 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
GALLINAS CREEK NEAR MONTEZUMA, NMStated 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
PECOS RIVER NEAR ANTON CHICO, NMStated 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
PECOS RIVER NEAR PECOS, NMStated 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
GALLINAS CREEK AT MONTEZUMA, NMStated 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
PECOS RIVER AT SANTA ROSA, NMStated 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 record5yes, 3 or more
Years spanned124yes, 20 or more
Values held1,718yes, 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), Pecos Headwaters gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-pecos-headwaters/

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 Pecos Headwaters 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 confidence2024-06-20

Source: USGS — National Water Information System, USGS site 08380500, 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.