The monitoring network within this area

Hydrionis holds 821 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
821
Values held
1904–2026
Record spans
Gauges within the Mojave huc8 subbasin
3 monitoring points, positioned as the publisher records them.
Gauges within the Mojave huc8 subbasinDEEP C NR HESPERIA CA, MOJAVE R A LO NARROWS NR VICTORVILLE CA, MOJAVE R A AFTON CADEEP C NR HESPERIA CAMOJAVE R A LO NARROWS NR VICTORVILLE CAMOJAVE R A AFTON CA

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 DEEP C NR HESPERIA CA
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1906–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at DEEP C NR HESPERIA CALargest measured flow of each year at DEEP C NR HESPERIA CA: DEEP C NR HESPERIA CA in m³/s, from 1906 to 2025.Hurricane Katrina water and sanitation collapse05001,0001,500m³/s19061931194519591973198619982013

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
PeriodDEEP C NR HESPERIA CA (m³/s)
1906306
1907196
1909178
19101,073
1911177
1914265
1915203
1916651
1918311
1920135
192162.3
19309.63
193145.3
1932224
19334.76
193578.2
193661.4
1937193
19381,320
193952.4
194073.9
194211.2
1943538
194413.9
1945180
194677.6
194823.8
19497.02
195020.0
19511.13
19534.08
1954208
19558.86
1956191
1957326
1958351
1959196
19603.17
196144.7
1962199
196317.8
196411.6
196512.5
1966436
196718.5
1969651
197015.8
1971252
1973193
197428.9
197514.2
1976143
197719.7
1978702
1979161
1980464
19813.68
198282.1
1983470
198423.1
1986145
198746.4
198819.5
198915.7
19902.46
1991252
1992297
1993510
1994109
1995326
1996156
1997142
1998462
19992.38
200054.4
20014.25
2003170
2004510
2006425
20072.32
2008173
200936.5
2010217
20129.20
20132.97
2014150
201654.4
2017109
201827.9
2019368
202059.5
20211.29
2023170
2024105
202571.4

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 held1906–2025
Completeness79.2% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 17 separate periods inside 1906–2025 hold no value. The longest runs from 1922 to 1929 — 8 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1906 and is not continuous from it: 120 years separate the first value from the last, and 79% 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 DEEP C NR HESPERIA CA, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1905–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above DEEP C NR HESPERIA CA, as a depthWater leaving the catchment above DEEP C NR HESPERIA CA, as a depth: DEEP C NR HESPERIA CA in mm, from 1905 to 2025.Hurricane Katrina water and sanitation collapse05001,000mm19051920194319581973198820032018

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
PeriodDEEP C NR HESPERIA CA (mm)
1905201
1906343
1907466
1908133
1909276
1910247
1911313
191290.0
191356.0
1914355
1915318
1916664
1917106
1918149
191945.0
1920189
1921286
193081.0
193152.0
1932229
193356.0
193452.0
1935125
193675.0
1937391
1938515
193999.0
1940109
1941350
194254.0
1943341
1944179
1945184
1946156
194742.0
194836.0
194959.0
195027.0
195126.0
1952196
195320.0
1954137
195542.0
195650.0
195798.0
1958336
195950.0
196033.0
196127.0
1962166
196322.0
196435.0
1965267
1966198
1967183
196848.0
1969779
197056.0
197195.0
197225.0
1973143
197466.0
197541.0
197664.0
197751.0
1978822
1979275
1980690
198136.0
1982183
1983535
198441.0
198556.0
1986109
198740.0
198839.0
198925.0
199022.0
1991113
1992183
19931,048
199473.0
1995496
1996106
199767.0
1998443
199924.0
200051.0
200145.0
200213.0
2003121
2004183
2005694
2006273
200721.0
2008131
2009112
2010520
2011242
201248.0
201323.0
201440.0
201516.0
201635.0
2017110
201826.0
2019244
202088.0
202147.0
202238.0
2023473
2024205
202589.0

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 held1905–2025
Completeness93.4% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • One period inside 1905–2025 holds no value: 1922 to 1929, 8 years with no reading. It is drawn as a break in the line and is never interpolated across.
ContinuityThe record begins in 1905 and is not continuous from it: 121 years separate the first value from the last, and 93% 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

Every gauge Hydrionis holds within this area

Gauges within the Mojave and what each holds
GaugeMeasuresValuesRecord
DEEP C NR HESPERIA CAburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3701904–2026
MOJAVE R A LO NARROWS NR VICTORVILLE CAburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2401931–2026
MOJAVE R A AFTON CAburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2111930–2026

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 — 18090208. 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
DEEP C NR HESPERIA CAStated 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
MOJAVE R A LO NARROWS NR VICTORVILLE CAStated 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
MOJAVE R A AFTON CAStated 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 record3yes, 3 or more
Years spanned123yes, 20 or more
Values held821no
Distinct measurements5yes, 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), Mojave gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-mojave/

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 Mojave 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 confidence2025-02-14

Source: USGS — National Water Information System, USGS site 10260500, 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.