The monitoring network within this area

Hydrionis holds 341 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
341
Values held
1909–2026
Record spans
Gauges within the Embarras huc8 subbasin
2 monitoring points, positioned as the publisher records them.
Gauges within the Embarras huc8 subbasinEMBARRAS RIVER AT STE. MARIE, IL, EMBARRAS RIVER NEAR OAKLAND, ILEMBARRAS RIVER AT STE. MARIE, ILEMBARRAS RIVER NEAR OAKLAND, IL

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 EMBARRAS RIVER AT STE. MARIE, IL
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1910–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at EMBARRAS RIVER AT STE. MARIE, ILLargest measured flow of each year at EMBARRAS RIVER AT STE. MARIE, IL: EMBARRAS RIVER AT STE. MARIE, IL in m³/s, from 1910 to 2025.Hurricane Katrina water and sanitation collapse05001,0001,5002,000m³/s19101929194219551970198420002015

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
PeriodEMBARRAS RIVER AT STE. MARIE, IL (m³/s)
1910261
1911371
1915411
1916399
1917668
1918236
1919228
1921198
1922796
1923470
1924292
1926269
19271,104
1929668
1930714
193197.1
1932236
1933637
1934103
1935357
1936239
1937490
19381,059
1939677
1940252
1941127
1942283
1943906
1944405
1945722
1946396
1947201
1948827
1949552
19501,269
1951561
1952241
1953144
195411.6
1955136
1956272
19571,127
1959549
1960357
19611,070
1962595
1963357
1964217
1965133
1966171
19671,056
1969674
1970561
1971235
1972211
1973371
1974617
1975552
1976362
1977211
1978470
1979702
1980214
1981212
1982623
1984779
1985799
1987155
1988473
1989422
1990663
1992300
1993597
1995694
1996903
1997459
1998445
1999665
2000253
20021,099
2003245
2004413
2005861
2006396
2007368
20081,710
2009719
2011765
2012263
2013680
2014326
2015360
2017966
2019357
2020753
2021283
2022436
2023419
2024225
2025708

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 held1910–2025
Completeness86.2% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 14 separate periods inside 1910–2025 hold no value. The longest runs from 1912 to 1914 — 3 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1910 and is not continuous from it: 116 years separate the first value from the last, and 86% 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 EMBARRAS RIVER AT STE. MARIE, IL, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1910–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above EMBARRAS RIVER AT STE. MARIE, IL, as a depthWater leaving the catchment above EMBARRAS RIVER AT STE. MARIE, IL, as a depth: EMBARRAS RIVER AT STE. MARIE, IL in mm, from 1910 to 2025.Hurricane Katrina water and sanitation collapse0200400600800mm19101928194319581973198820032018

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
PeriodEMBARRAS RIVER AT STE. MARIE, IL (mm)
1910236
1911346
1915300
1916264
1917234
1918325
1919280
1920213
1921240
1922307
1923265
1924322
1925153
1926347
1927673
1928288
1929444
1930249
1931136
1932181
1933380
1934144
1935284
1936155
1937343
1938333
1939311
1940100
1941138
1942348
1943324
1944178
1945379
1946295
1947239
1948259
1949399
1950557
1951388
1952254
1953121
195410.0
1955146
1956155
1957533
1958321
1959210
1960179
1961249
1962299
196390.0
1964136
1965133
1966190
1967340
1968292
1969341
1970223
1971179
1972232
1973490
1974552
1975413
1976156
1977168
1978310
1979444
1980177
1981263
1982537
1983331
1984368
1985483
1986159
1987150
1988212
1989280
1990395
1991270
1992317
1993644
1994253
1995224
1996405
1997255
1998385
1999303
2000264
2001312
2002429
2003166
2004363
2005262
2006282
2007252
2008580
2009559
2010301
2011477
2012128
2013409
2014294
2015374
2016305
2017315
2018404
2019479
2020479
2021392
2022327
2023181
2024204
2025210

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 held1910–2025
Completeness97.4% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • One period inside 1910–2025 holds no value: 1912 to 1914, 3 years with no reading. It is drawn as a break in the line and is never interpolated across.
ContinuityThe record begins in 1910 and is not continuous from it: 116 years separate the first value from the last, and 97% 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 Embarras and what each holds
GaugeMeasuresValuesRecord
EMBARRAS RIVER AT STE. MARIE, ILcatchment area, annual maximum river flow, mean river flow, mean river flow, water year3401909–2026
EMBARRAS RIVER NEAR OAKLAND, ILcatchment area12026–2026

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 — 05120112. 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
EMBARRAS RIVER AT STE. MARIE, ILStated 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
EMBARRAS RIVER NEAR OAKLAND, ILStated 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 2 of them, which makes it a profile, not indexed.

Information-gain signals held for this water body
SignalHeldCounts
Gauges holding a real record1no
Years spanned118yes, 20 or more
Values held341no
Distinct measurements4yes, 2 or more
Publishers measuring it1no
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), Embarras gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-embarras/

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 Embarras 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 confidence2025-04-06

Source: USGS — National Water Information System, USGS site 03345500, 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.