The monitoring network within this area

Hydrionis holds 1,585 values from 6 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.

6
Gauges
1,585
Values held
1911–2026
Record spans
Gauges within the Upper Yuba huc8 subbasin
6 monitoring points, positioned as the publisher records them.
Gauges within the Upper Yuba huc8 subbasinMILTON-BOWMAN TUNNEL OUTLET NR GRANITEVILLE CA, OREGON C NR NORTH SAN JUAN CA, BOWMAN-SPAULDING CN INTAKE NR GRANITEVILLE CA, CANYON C BL BOWMAN LK CA, M YUBA R A MILTON CA, M YUBA R NR NORTH SAN JUAN CAMILTON-BOWMAN TUNNEL OUTLET NR GRANITEVILLE CAOREGON C NR NORTH SAN JUAN CABOWMAN-SPAULDING CN INTAKE NR GRANITEVILLE CACANYON C BL BOWMAN LK CAM YUBA R A MILTON CAM YUBA R NR NORTH SAN JUAN 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 CANYON C BL BOWMAN LK CA
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1927–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at CANYON C BL BOWMAN LK CALargest measured flow of each year at CANYON C BL BOWMAN LK CA: CANYON C BL BOWMAN LK CA in m³/s, from 1927 to 2025.Hurricane Katrina water and sanitation collapse050100150200m³/s19271939195019631975199120022015

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
PeriodCANYON C BL BOWMAN LK CA (m³/s)
192722.5
19283.06
19297.39
193024.1
19311.44
193225.1
19332.41
193523.3
193641.3
193724.6
193830.9
19390.510
194025.0
194121.9
194220.0
194357.5
19441.16
194524.2
194630.9
19471.64
194841.9
19491.76
195043.0
195234.0
195326.3
19546.80
19552.44
195638.8
195725.5
195826.4
19594.33
196020.8
196220.8
196340.8
196424.5
19650.651
196719.4
19681.19
196931.7
1970106
197140.8
19720.934
19738.07
197417.3
197515.2
19770.510
19792.04
19807.08
19811.39
198237.9
198325.1
19841.05
1986112
19871.59
19892.83
19914.11
19922.10
19939.71
19941.25
199512.9
199689.2
1997156
199836.2
19996.60
20009.43
20011.36
20021.70
200318.3
20041.47
200521.6
20072.18
20085.04
200910.6
201015.7
201111.7
201228.6
20142.24
20152.29
201617.8
2017109
201858.0
201929.7
20207.82
20213.54
20228.41
202332.0
202424.2
202520.1

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 held1927–2025
Completeness88.9% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 11 separate periods inside 1927–2025 hold no value. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1927 and is not continuous from it: 99 years separate the first value from the last, and 89% 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 CANYON C BL BOWMAN LK 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. 1928–2024.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above CANYON C BL BOWMAN LK CA, as a depthWater leaving the catchment above CANYON C BL BOWMAN LK CA, as a depth: CANYON C BL BOWMAN LK CA in mm, from 1928 to 2024.Hurricane Katrina water and sanitation collapse01,0002,0003,000mm19281941195419671980199320062019

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
PeriodCANYON C BL BOWMAN LK CA (mm)
1928121
192944.0
1930275
193112.0
1932706
193322.0
193410.0
1935508
1936373
1937214
1938989
193921.0
1940957
1941820
19421,078
1943992
194419.0
1945401
1946513
194712.0
1948453
194915.0
19501,155
1951579
19521,743
1953733
1954206
195533.0
19561,056
1957552
1958587
195937.0
1960244
196113.0
1962258
19631,116
1964761
19651,652
196653.0
1967465
196848.0
19691,009
1970543
1971261
197267.0
1973144
1974465
1975138
197632.0
197713.0
197838.0
197941.0
1980138
1981116
19821,000
19831,008
1984243
198562.0
19861,033
198758.0
198855.0
198994.0
199059.0
199154.0
199261.0
1993443
199452.0
1995998
1996969
1997805
1998982
1999381
2000173
200160.0
200263.0
2003420
200476.0
2005591
20061,468
200774.0
200880.0
2009313
2010735
2011793
2012293
201372.0
201465.0
201573.0
20161,284
20172,587
2018783
20191,605
2020156
202176.0
2022145
20231,547
2024878

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 held1928–2024
Completeness100.0% of the periods in that span are held.
ContinuityContinuous: every year from 1928 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.

1,818
Fullest snowpack recorded at Css Lab, in 2023 (mm of water)
152
Thinnest, in 2015 (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 Css Lab
Water years 1984–2026. Each point is the fullest month of that snow season.
Peak snowpack at Css LabPeak snowpack at Css Lab: Css Lab in mm, from 1984 to 2026.05001,0001,5002,000mm19841990199620022008201420202026Css Lab 1984: 990 mmCss Lab 1985: 728 mmCss Lab 1986: 1,197 mmCss Lab 1987: 567 mmCss Lab 1988: 461 mmCss Lab 1989: 784 mmCss Lab 1990: 477 mmCss Lab 1991: 415 mmCss Lab 1992: 418 mmCss Lab 1993: 1,288 mmCss Lab 1994: 547 mmCss Lab 1995: 1,552 mmCss Lab 1996: 879 mmCss Lab 1997: 1,160 mmCss Lab 1998: 1,250 mmCss Lab 1999: 1,320 mmCss Lab 2000: 1,085 mmCss Lab 2001: 546 mmCss Lab 2002: 798 mmCss Lab 2003: 793 mmCss Lab 2004: 846 mmCss Lab 2005: 1,040 mmCss Lab 2006: 1,330 mmCss Lab 2007: 606 mmCss Lab 2008: 909 mmCss Lab 2009: 914 mmCss Lab 2010: 1,043 mmCss Lab 2011: 1,749 mmCss Lab 2012: 557 mmCss Lab 2013: 482 mmCss Lab 2014: 203 mmCss Lab 2015: 152 mmCss Lab 2016: 874 mmCss Lab 2017: 1,674 mmCss Lab 2018: 393 mmCss Lab 2019: 1,587 mmCss Lab 2020: 425 mmCss Lab 2021: 697 mmCss Lab 2022: 700 mmCss Lab 2023: 1,818 mmCss Lab 2024: 950 mmCss Lab 2025: 721 mmCss Lab 2026: 378 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
PeriodCss Lab (mm)
1984990
1985728
19861,197
1987567
1988461
1989784
1990477
1991415
1992418
19931,288
1994547
19951,552
1996879
19971,160
19981,250
19991,320
20001,085
2001546
2002798
2003793
2004846
20051,040
20061,330
2007606
2008909
2009914
20101,043
20111,749
2012557
2013482
2014203
2015152
2016874
20171,674
2018393
20191,587
2020425
2021697
2022700
20231,818
2024950
2025721
2026378

Why the snow is not read against the river here

MILTON-BOWMAN TUNNEL OUTLET NR GRANITEVILLE CA measures a tunnel, not a natural channel. What passes through it is an operating decision — how much was diverted, and when — so comparing it with what the sky or the mountain delivered would describe the operator rather than the hydrology.

Every gauge Hydrionis holds within this area

Gauges within the Upper Yuba and what each holds
GaugeMeasuresValuesRecord
CANYON C BL BOWMAN LK CAburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3311927–2026
MILTON-BOWMAN TUNNEL OUTLET NR GRANITEVILLE CAburned area within 50 km, mean river flow, mean river flow, water year2291928–2024
BOWMAN-SPAULDING CN INTAKE NR GRANITEVILLE CAburned area within 50 km, mean river flow, mean river flow, water year2251927–2024
OREGON C NR NORTH SAN JUAN CAburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2081911–2026
M YUBA R A MILTON CAcatchment area, annual maximum river flow361926–2026
M YUBA R NR NORTH SAN JUAN CAcatchment area, annual maximum river flow351912–2026

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 — 18020125. 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
CANYON C BL BOWMAN LK 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
MILTON-BOWMAN TUNNEL OUTLET NR GRANITEVILLE 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
BOWMAN-SPAULDING CN INTAKE NR GRANITEVILLE 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
OREGON C NR NORTH SAN JUAN 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
M YUBA R A MILTON 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
M YUBA R NR NORTH SAN JUAN 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 5 of them, which makes it a full profile.

Information-gain signals held for this water body
SignalHeldCounts
Gauges holding a real record4yes, 3 or more
Years spanned116yes, 20 or more
Values held1,585yes, 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), Upper Yuba gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-upper-yuba/

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 Yuba 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 confidence2025-04-18

Source: USGS — National Water Information System, USGS site 11416500, 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.