The monitoring network within this area

Hydrionis holds 477 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
477
Values held
1914–2026
Record spans
Gauges within the Upper Gila-San Carlos Reservoir huc8 subbasin
2 monitoring points, positioned as the publisher records them.
Gauges within the Upper Gila-San Carlos Reservoir huc8 subbasinGILA RIVER AT HEAD OF SAFFORD VALLEY, NR SOLOMON,, GILA RIVER AT CALVA, AZGILA RIVER AT HEAD OF SAFFORD VALLEY, NR SOLOMON,GILA RIVER AT CALVA, AZ

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 GILA RIVER AT HEAD OF SAFFORD VALLEY, NR SOLOMON,
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1914–2024.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at GILA RIVER AT HEAD OF SAFFORD VALLEY, NR SOLOMON,Largest measured flow of each year at GILA RIVER AT HEAD OF SAFFORD VALLEY, NR SOLOMON,: GILA RIVER AT HEAD OF SAFFORD VALLEY, NR SOLOMON, in m³/s, from 1914 to 2024.Hurricane Katrina water and sanitation collapse01,0002,0003,0004,000m³/s19141930194319571972198820022015

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 recordA 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 collapseFlood2005-08-292005-09-30Documented record
Compiled record

Not shown on this chart

  • The 1976 droughtThis 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 droughtThis event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • Yorkshire droughtThis 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 PauloThis 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 ZeroThis event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • European droughtThis 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
PeriodGILA RIVER AT HEAD OF SAFFORD VALLEY, NR SOLOMON, (m³/s)
1914255
19162,832
191876.5
1919425
1921445
1922107
1923357
1925450
1926160
1927264
192891.5
1929360
1930286
1931297
1932680
1933272
1934651
1935157
1936227
1937671
1938133
1939209
1940279
1941903
1943189
1944447
1945136
1947262
194871.9
1949714
195035.1
1951120
1952558
195386.1
1954279
1955331
1957169
1958257
1959223
1960473
1961136
1962456
1964280
1965136
1967985
196969.7
197063.7
1971289
19722,333
197492.9
1975991
197696.3
197771.9
1978612
1980716
1981198
1983320
19841,705
1985218
198685.5
1988221
199063.4
1991742
1992507
19932,441
199449.8
19951,767
1996212
1997479
1998140
1999233
200014.3
2002134
200371.4
20051,104
2006166
200794.0
2008470
200921.1
2010306
201132.0
201281.8
2013776
2014244
2015286
2016103
2017191
2018122
2019191
2021118
2022580
2023314
202434.8

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 held19142024
Completeness83.8% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 18 separate periods inside 1914–2024 hold no value. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1914 and is not continuous from it: 111 years separate the first value from the last, and 84% of the years between them are held. The span is not the record.
Last read from the publisher2026-08-31
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 GILA RIVER AT HEAD OF SAFFORD VALLEY, NR SOLOMON,, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1921–2024.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above GILA RIVER AT HEAD OF SAFFORD VALLEY, NR SOLOMON,, as a depthWater leaving the catchment above GILA RIVER AT HEAD OF SAFFORD VALLEY, NR SOLOMON,, as a depth: GILA RIVER AT HEAD OF SAFFORD VALLEY, NR SOLOMON, in mm, from 1921 to 2024.Hurricane Katrina water and sanitation collapse0255075100mm19211937195019631976198920022015

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 recordA 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 collapseFlood2005-08-292005-09-30Documented record
Compiled record

Not shown on this chart

  • The 1976 droughtThis 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 droughtThis event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • Yorkshire droughtThis 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 PauloThis 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 ZeroThis event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • European droughtThis 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
PeriodGILA RIVER AT HEAD OF SAFFORD VALLEY, NR SOLOMON, (mm)
192118.0
19228.00
192326.0
192417.0
192515.0
192620.0
192717.0
192811.0
192915.0
193014.0
193123.0
193228.0
193613.0
193725.0
193810.0
193910.0
194018.0
194156.0
194213.0
19439.00
19449.00
194513.0
19467.00
19476.00
19489.00
194934.0
19505.00
19515.00
195220.0
19535.00
195412.0
195510.0
19563.00
195714.0
195828.0
195911.0
196017.0
196110.0
196225.0
196317.0
19649.00
196524.0
196626.0
196716.0
196840.0
19697.00
19707.00
197111.0
197231.0
197340.0
19747.00
197521.0
19769.00
19778.00
197849.0
197945.0
198027.0
19819.00
198217.0
198374.0
198427.0
198550.0
198622.0
198720.0
198827.0
19897.00
199010.0
199141.0
199248.0
199394.0
199423.0
199537.0
199612.0
199720.0
199821.0
199913.0
200020.0
200111.0
20026.00
20037.00
200411.0
200538.0
200622.0
200715.0
200821.0
20096.00
201028.0
20116.00
20126.00
201320.0
201411.0
201516.0
201612.0
201722.0
20186.00
201916.0
202016.0
20218.00
202227.0
202324.0
20249.00

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 held19212024
Completeness97.1% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • One period inside 1921–2024 holds no value: 1933 to 1935, 3 years with no reading. It is drawn as a break in the line and is never interpolated across.
ContinuityThe record begins in 1921 and is not continuous from it: 104 years separate the first value from the last, and 97% of the years between them are held. The span is not the record.
Last read from the publisher2026-08-24
RedistributionPermitted by the upstream licences
Commercial reusePermitted by the upstream licences. No Hydrionis access tier can widen this.
MethodologyHow this was produced

Every gauge Hydrionis holds within this area

Gauges within the Upper Gila-San Carlos Reservoir and what each holds
GaugeMeasuresValuesRecord
GILA RIVER AT HEAD OF SAFFORD VALLEY, NR SOLOMON,burned area within 50 km, catchment area, annual maximum river flow, mean river flow2491914–2026
GILA RIVER AT CALVA, AZburned area within 50 km, catchment area, annual maximum river flow, mean river flow2281916–2026

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 — 15040005. 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
GILA RIVER AT HEAD OF SAFFORD VALLEY, NR SOLOMON,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/42026-08-26
GILA RIVER AT CALVA, AZStated 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/42026-08-26

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 3 of them, which makes it a full profile.

Information-gain signals held for this water body
SignalHeldCounts
Gauges holding a real record2no
Years spanned113yes, 20 or more
Values held477no
Distinct measurements4yes, 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), Upper Gila-San Carlos Reservoir gauge records, accessed 2026-09-02, hydrionis.com/waters/united-states-upper-gila-san-carlos-reservoir/

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 Upper Gila-San Carlos Reservoir 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 confidence2024-04-03

Source: USGSNational Water Information System, USGS site 09448500, 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 31 August 2026.