The monitoring network within this area

Hydrionis holds 1,164 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
1,164
Values held
1913–2026
Record spans
Gauges within the Rio Grande-Santa Fe huc8 subbasin
2 monitoring points, positioned as the publisher records them.
Gauges within the Rio Grande-Santa Fe huc8 subbasinSANTA FE RIVER NEAR SANTA FE, NM, RIO GRANDE AT SAN FELIPE, NMSANTA FE RIVER NEAR SANTA FE, NMRIO GRANDE AT SAN FELIPE, 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 SANTA FE RIVER NEAR SANTA FE, NM
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1913–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at SANTA FE RIVER NEAR SANTA FE, NMLargest measured flow of each year at SANTA FE RIVER NEAR SANTA FE, NM: SANTA FE RIVER NEAR SANTA FE, NM in m³/s, from 1913 to 2025.Hurricane Katrina water and sanitation collapse02040m³/s19131927193919651979199220072020

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
PeriodSANTA FE RIVER NEAR SANTA FE, NM (m³/s)
19132.46
19146.40
19154.02
19162.66
19180.793
19194.59
19202.66
192142.5
19220.708
19241.84
19252.27
19262.83
19271.42
19284.81
192917.0
19301.59
19313.94
19321.33
19331.08
19340.266
19351.87
19363.17
19372.38
19380.623
19390.878
19400.878
19414.67
194211.8
19431.56
19441.05
19451.59
19461.13
19610.623
19622.32
19632.61
19640.340
19656.17
19670.708
19682.49
19691.93
19700.396
19710.481
19720.453
19734.96
19740.340
19751.05
19760.595
19780.793
19798.69
19802.38
19810.368
19820.311
19833.91
19841.84
19854.93
19861.10
19872.89
19881.27
19900.906
19912.38
19923.17
19932.92
19942.61
19953.37
19960.765
19972.58
19980.850
19990.991
20030.510
20040.821
20052.04
20061.73
20071.42
20081.22
20091.30
20102.35
20110.510
20120.340
20130.311
20151.73
20160.481
20171.37
20182.63
20191.10
20200.311
20210.314
20220.334
20230.748
20240.323
20250.487

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 held1913–2025
Completeness79.6% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 8 separate periods inside 1913–2025 hold no value. The longest runs from 1947 to 1960 — 14 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1913 and is not continuous from it: 113 years separate the first value from the last, and 80% 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 SANTA FE RIVER NEAR SANTA FE, 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. 1914–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above SANTA FE RIVER NEAR SANTA FE, NM, as a depthWater leaving the catchment above SANTA FE RIVER NEAR SANTA FE, NM, as a depth: SANTA FE RIVER NEAR SANTA FE, NM in mm, from 1914 to 2025.Hurricane Katrina water and sanitation collapse0200400600mm19141932194619601974198820022016

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
PeriodSANTA FE RIVER NEAR SANTA FE, NM (mm)
1914231
1915328
1916346
191767.0
1918129
1919521
1920183
1921436
192287.0
1923132
1924196
192552.0
1926239
1931205
1932177
193375.0
193449.0
1935167
1936171
1937186
193878.0
1939131
1940138
1941417
1942265
1943109
1944133
1945178
194688.0
194777.0
194894.0
1949184
195074.0
195129.0
195290.0
195385.0
195459.0
195552.0
195638.0
1957121
1958305
195975.0
1960135
1961106
1962134
1963127
196466.0
1965154
1966153
196788.0
1968127
1969151
197089.0
197168.0
197275.0
1973292
197469.0
1975147
197677.0
197757.0
1978121
1979260
1980181
198156.0
1982106
1983290
1984138
1985316
1986170
1987256
1988124
198987.0
199096.0
1991208
1992255
1993256
1994197
1995208
199683.0
1997203
1998158
1999115
200089.0
2001123
200219.0
200361.0
200487.0
2005237
200674.0
2007155
2008138
2009143
2010174
201159.0
201281.0
201345.0
2014127
2015140
201695.0
2017118
201847.0
2019220
202089.0
202165.0
202299.0
2023183
202496.0
2025100

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 held1914–2025
Completeness96.4% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • One period inside 1914–2025 holds no value: 1927 to 1930, 4 years with no reading. It is drawn as a break in the line and is never interpolated across.
ContinuityThe record begins in 1914 and is not continuous from it: 112 years separate the first value from the last, and 96% 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

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

650
Fullest snowpack recorded at Santa Fe, in 2005 (mm of water)
30
Thinnest, in 2006 (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 Santa Fe
Water years 1997–2026. Each point is the fullest month of that snow season.
Peak snowpack at Santa FePeak snowpack at Santa Fe: Santa Fe in mm, from 1997 to 2026.0200400600800mm19972001200520092013201720212025Santa Fe 1997: 547 mmSanta Fe 1998: 509 mmSanta Fe 1999: 238 mmSanta Fe 2000: 238 mmSanta Fe 2001: 397 mmSanta Fe 2002: 140 mmSanta Fe 2003: 454 mmSanta Fe 2004: 402 mmSanta Fe 2005: 650 mmSanta Fe 2006: 30.0 mmSanta Fe 2007: 354 mmSanta Fe 2008: 520 mmSanta Fe 2009: 407 mmSanta Fe 2010: 508 mmSanta Fe 2011: 205 mmSanta Fe 2012: 295 mmSanta Fe 2013: 242 mmSanta Fe 2014: 175 mmSanta Fe 2015: 320 mmSanta Fe 2016: 460 mmSanta Fe 2017: 360 mmSanta Fe 2018: 99.0 mmSanta Fe 2019: 491 mmSanta Fe 2020: 378 mmSanta Fe 2021: 189 mmSanta Fe 2022: 249 mmSanta Fe 2023: 471 mmSanta Fe 2024: 443 mmSanta Fe 2025: 139 mmSanta Fe 2026: 159 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
PeriodSanta Fe (mm)
1997547
1998509
1999238
2000238
2001397
2002140
2003454
2004402
2005650
200630.0
2007354
2008520
2009407
2010508
2011205
2012295
2013242
2014175
2015320
2016460
2017360
201899.0
2019491
2020378
2021189
2022249
2023471
2024443
2025139
2026159

Read against the river

Santa Fe and SANTA FE RIVER NEAR SANTA FE, NM both sit in this drainage area, and their records overlap by 28 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 Rio Grande-Santa Fe and what each holds
GaugeMeasuresValuesRecord
SANTA FE RIVER NEAR SANTA FE, NMburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3491913–2026
RIO GRANDE AT SAN FELIPE, NMcatchment area, annual maximum river flow951927–2026

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 — 13020201. 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
SANTA FE RIVER NEAR SANTA FE, 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
RIO GRANDE AT SAN FELIPE, 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 4 of them, which makes it a full profile.

Information-gain signals held for this water body
SignalHeldCounts
Gauges holding a real record2no
Years spanned114yes, 20 or more
Values held1,164yes, 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), Rio Grande-Santa Fe gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-rio-grande-santa-fe/

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 Rio Grande-Santa Fe 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 confidence2025-09-05

Source: USGS — National Water Information System, USGS site 08316000, 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.