The monitoring network within this area

Hydrionis holds 1,490 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
1,490
Values held
1911–2026
Record spans
Gauges within the Donner und Blitzen huc8 subbasin
2 monitoring points, positioned as the publisher records them.
Gauges within the Donner und Blitzen huc8 subbasinDONNER UND BLITZEN RIVER NR FRENCHGLEN OR, BRIDGE CREEK NR FRENCHGLEN, OREG.DONNER UND BLITZEN RIVER NR FRENCHGLEN ORBRIDGE CREEK NR FRENCHGLEN, OREG.

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 DONNER UND BLITZEN RIVER NR FRENCHGLEN OR
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1911–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at DONNER UND BLITZEN RIVER NR FRENCHGLEN ORLargest measured flow of each year at DONNER UND BLITZEN RIVER NR FRENCHGLEN OR: DONNER UND BLITZEN RIVER NR FRENCHGLEN OR in m³/s, from 1911 to 2025.Hurricane Katrina water and sanitation collapse050100m³/s19111939195219641977198920012014

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
PeriodDONNER UND BLITZEN RIVER NR FRENCHGLEN OR (m³/s)
191151.0
191238.5
191339.1
191424.2
191558.3
191651.5
191812.5
191947.3
192032.3
192162.3
19307.82
193730.6
193944.7
194044.5
194123.6
194264.3
194334.8
194415.4
194536.2
194718.3
194848.1
194928.9
195022.5
195156.6
195264.0
195377.9
195435.1
195530.0
195660.6
195772.5
195840.2
19599.37
196029.2
196113.3
196224.0
196339.6
196442.5
196617.8
196734.0
196821.9
196967.4
197077.0
197177.9
197280.1
197319.8
197454.4
197530.9
197630.0
197730.6
1978121
197942.2
198034.8
198147.3
198266.3
198366.8
198447.0
198534.3
198686.6
198720.3
198820.8
198997.7
199013.0
199156.6
19926.68
199399.7
199419.1
199561.7
199631.7
199784.7
199888.1
199932.6
200017.3
200130.3
200223.5
200345.3
200421.5
2005118
200723.9
200831.1
200970.8
201061.2
201168.8
201220.4
201313.1
201426.2
201544.7
201631.1
201727.0
20189.23
201947.3
202017.4
202111.0
202232.6
202367.1
202429.7
202546.4

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 held1911–2025
Completeness83.5% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 7 separate periods inside 1911–2025 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 1911 and is not continuous from it: 115 years separate the first value from the last, and 83% 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 DONNER UND BLITZEN RIVER NR FRENCHGLEN OR, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1912–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above DONNER UND BLITZEN RIVER NR FRENCHGLEN OR, as a depthWater leaving the catchment above DONNER UND BLITZEN RIVER NR FRENCHGLEN OR, as a depth: DONNER UND BLITZEN RIVER NR FRENCHGLEN OR in mm, from 1912 to 2025.Hurricane Katrina water and sanitation collapse0200400mm19121945195719691981199320052017

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
PeriodDONNER UND BLITZEN RIVER NR FRENCHGLEN OR (mm)
1912315
1915192
1918147
1919182
1920227
1938248
1939159
1940188
1941201
1942291
1943265
1944153
1945287
1946173
1947134
1948242
1949150
1950183
1951212
1952348
1953217
1954165
1955183
1956261
1957292
1958255
1959103
1960175
1961109
1962157
1963167
1964209
1965219
196695.0
1967194
196899.0
1969265
1970203
1971275
1972250
1973154
1974205
1975289
1976207
1977111
1978280
1979287
1980269
1981227
1982285
1983434
1984469
1985211
1986282
1987158
1988134
1989284
1990114
1991178
199277.0
1993318
1994128
1995285
1996267
1997264
1998377
1999278
2000149
2001142
2002163
2003169
2004190
2005242
2006262
2007154
2008187
2009190
2010318
2011450
2012147
2013130
2014141
2015127
2016180
2017214
2018106
2019293
2020151
2021126
2022129
2023249
2024260
2025314

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 held1912–2025
Completeness81.6% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 3 separate periods inside 1912–2025 hold no value. The longest runs from 1921 to 1937 — 17 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1912 and is not continuous from it: 114 years separate the first value from the last, and 82% 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.

1,378
Fullest snowpack recorded at Fish Creek, in 1983 (mm of water)
257
Thinnest, in 2026 (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 Fish Creek
Water years 1980–2026. Each point is the fullest month of that snow season.
Peak snowpack at Fish CreekPeak snowpack at Fish Creek: Fish Creek in mm, from 1980 to 2026.05001,0001,500mm19801986199219982004201020162022Fish Creek 1980: 901 mmFish Creek 1981: 442 mmFish Creek 1982: 972 mmFish Creek 1983: 1,378 mmFish Creek 1984: 1,327 mmFish Creek 1985: 651 mmFish Creek 1986: 896 mmFish Creek 1987: 516 mmFish Creek 1988: 489 mmFish Creek 1989: 1,028 mmFish Creek 1990: 338 mmFish Creek 1991: 705 mmFish Creek 1992: 391 mmFish Creek 1993: 1,092 mmFish Creek 1994: 433 mmFish Creek 1995: 1,147 mmFish Creek 1996: 876 mmFish Creek 1997: 1,003 mmFish Creek 1998: 977 mmFish Creek 1999: 1,036 mmFish Creek 2000: 575 mmFish Creek 2001: 493 mmFish Creek 2002: 674 mmFish Creek 2003: 646 mmFish Creek 2004: 789 mmFish Creek 2005: 625 mmFish Creek 2006: 1,147 mmFish Creek 2007: 649 mmFish Creek 2008: 705 mmFish Creek 2009: 615 mmFish Creek 2010: 820 mmFish Creek 2011: 1,271 mmFish Creek 2012: 514 mmFish Creek 2013: 736 mmFish Creek 2014: 615 mmFish Creek 2015: 500 mmFish Creek 2016: 864 mmFish Creek 2017: 1,048 mmFish Creek 2018: 500 mmFish Creek 2019: 836 mmFish Creek 2020: 639 mmFish Creek 2021: 692 mmFish Creek 2022: 528 mmFish Creek 2023: 873 mmFish Creek 2024: 1,092 mmFish Creek 2025: 1,322 mmFish Creek 2026: 257 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
PeriodFish Creek (mm)
1980901
1981442
1982972
19831,378
19841,327
1985651
1986896
1987516
1988489
19891,028
1990338
1991705
1992391
19931,092
1994433
19951,147
1996876
19971,003
1998977
19991,036
2000575
2001493
2002674
2003646
2004789
2005625
20061,147
2007649
2008705
2009615
2010820
20111,271
2012514
2013736
2014615
2015500
2016864
20171,048
2018500
2019836
2020639
2021692
2022528
2023873
20241,092
20251,322
2026257

Read against the river

Fish Creek and DONNER UND BLITZEN RIVER NR FRENCHGLEN OR both sit in this drainage area, and their records overlap by 45 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 Donner und Blitzen and what each holds
GaugeMeasuresValuesRecord
DONNER UND BLITZEN RIVER NR FRENCHGLEN ORburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3231911–2026
BRIDGE CREEK NR FRENCHGLEN, OREG.catchment area, annual maximum river flow401911–2026

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 — 17120003. 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
DONNER UND BLITZEN RIVER NR FRENCHGLEN ORStated 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
BRIDGE CREEK NR FRENCHGLEN, OREG.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/42026-10-02

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 record1no
Years spanned116yes, 20 or more
Values held1,490yes, 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), Donner und Blitzen gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-donner-und-blitzen/

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 Donner und Blitzen 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 confidence2025-02-24

Source: USGS — National Water Information System, USGS site 10396000, 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.