The monitoring network within this area

Hydrionis holds 790 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
790
Values held
1917–2026
Record spans
Gauges within the Roseau huc8 subbasin
3 monitoring points, positioned as the publisher records them.
Gauges within the Roseau huc8 subbasinROSEAU RIVER AT ROSS, MN, ROSEAU RIVER BELOW STATE DITCH 51 NR CARIBOU, MN, SPRAGUE CREEK NEAR SPRAGUE, MANITOBA, CANADAROSEAU RIVER AT ROSS, MNROSEAU RIVER BELOW STATE DITCH 51 NR CARIBOU, MNSPRAGUE CREEK NEAR SPRAGUE, MANITOBA, CANADA

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 ROSEAU RIVER BELOW STATE DITCH 51 NR CARIBOU, MN
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1917–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at ROSEAU RIVER BELOW STATE DITCH 51 NR CARIBOU, MNLargest measured flow of each year at ROSEAU RIVER BELOW STATE DITCH 51 NR CARIBOU, MN: ROSEAU RIVER BELOW STATE DITCH 51 NR CARIBOU, MN in m³/s, from 1917 to 2025.Hurricane Katrina water and sanitation collapse050100m³/s19171932194619611974198720002016

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
PeriodROSEAU RIVER BELOW STATE DITCH 51 NR CARIBOU, MN (m³/s)
191741.6
192048.7
192156.1
192238.5
192384.4
192434.8
192560.6
192653.8
192789.8
192847.3
192927.8
193039.1
193132.3
193248.4
193338.2
193412.0
193628.9
193738.5
193849.6
19399.63
194023.6
194147.0
194258.6
194348.1
194436.0
194549.8
194644.2
194750.4
194869.7
194941.9
1950116
195162.3
195322.6
195530.6
195665.1
195750.7
195824.8
195944.5
196046.7
196117.3
196258.6
196342.8
196440.5
196576.2
196688.3
196768.2
196852.7
196970.2
197083.3
197149.3
197247.9
197320.4
197477.0
197571.9
197637.7
197710.8
197864.0
197984.4
198029.7
198121.0
198247.0
198339.6
198434.8
198542.2
198667.1
198746.2
198828.3
198937.9
199011.3
199137.9
199269.9
199349.0
199436.8
199566.5
199694.9
199794.0
199845.0
199973.3
200043.0
200182.7
2002122
200322.1
200498.5
200569.4
200684.1
200991.7
201062.9
201185.0
201358.3
201473.1
201548.1
201660.9
201767.7
201836.0
201949.0
202114.5
202289.8
202366.0
202447.9
202523.9

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 held1917–2025
Completeness91.7% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 7 separate periods inside 1917–2025 hold no value. The longest runs from 1918 to 1919 — 2 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1917 and is not continuous from it: 109 years separate the first value from the last, and 92% 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 ROSEAU RIVER AT ROSS, MN, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1929–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above ROSEAU RIVER AT ROSS, MN, as a depthWater leaving the catchment above ROSEAU RIVER AT ROSS, MN, as a depth: ROSEAU RIVER AT ROSS, MN in mm, from 1929 to 2025.Hurricane Katrina water and sanitation collapse0100200300mm19291941195319651977198920062018

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
PeriodROSEAU RIVER AT ROSS, MN (mm)
192934.0
193059.0
193125.0
193253.0
193339.0
193410.0
193530.0
193630.0
193784.0
193879.0
193910.0
194019.0
1941110
1942122
1943115
194487.0
1945115
194668.0
194792.0
1948106
194955.0
1950246
1951109
195230.0
195335.0
195456.0
195550.0
1956141
1957142
195828.0
195969.0
196051.0
196121.0
1962145
196368.0
1964102
1965170
1966193
1967116
1968178
1969116
1970190
197168.0
197266.0
197341.0
1974165
1975138
197635.0
197720.0
197894.0
1979122
198021.0
198138.0
198282.0
198378.0
198452.0
1985167
1986131
198745.0
198813.0
198954.0
199014.0
1996192
1997170
1998101
1999197
2000133
2001180
2002221
200350.0
2004266
2005200
2006110
200785.0
200898.0
2009203
2010177
2011160
201221.0
201392.0
2014154
2015105
2016173
2017113
201842.0
2019216
2020140
202117.0
2022214
202490.0
202559.0

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 held1929–2025
Completeness93.8% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 2 separate periods inside 1929–2025 hold no value. The longest runs from 1991 to 1995 — 5 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1929 and is not continuous from it: 97 years separate the first value from the last, and 94% 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 Roseau and what each holds
GaugeMeasuresValuesRecord
ROSEAU RIVER AT ROSS, MNburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3081928–2026
SPRAGUE CREEK NEAR SPRAGUE, MANITOBA, CANADAburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2471928–2026
ROSEAU RIVER BELOW STATE DITCH 51 NR CARIBOU, MNcatchment area, annual maximum river flow, mean river flow, mean river flow, water year2351917–2026

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 — 09020314. 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
ROSEAU RIVER AT ROSS, MNStated 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
SPRAGUE CREEK NEAR SPRAGUE, MANITOBA, CANADAStated 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
ROSEAU RIVER BELOW STATE DITCH 51 NR CARIBOU, MNStated 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 spanned110yes, 20 or more
Values held790no
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), Roseau gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-roseau/

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 Roseau 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 confidence2025-05-06

Source: USGS — National Water Information System, USGS site 05107500, 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.