The monitoring network within this area

Hydrionis holds 844 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
844
Values held
1920–2026
Record spans
Gauges within the Saint Croix River huc8 subbasin
3 monitoring points, positioned as the publisher records them.
Gauges within the Saint Croix River huc8 subbasinSt. Croix River at Vanceboro, Maine, Grand Lake Stream at Grand Lake Stream, Maine, ST. CROIX RIVER NEAR BAILEYVILLE, MESt. Croix River at Vanceboro, MaineGrand Lake Stream at Grand Lake Stream, MaineST. CROIX RIVER NEAR BAILEYVILLE, ME

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 Grand Lake Stream at Grand Lake Stream, Maine
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1929–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at Grand Lake Stream at Grand Lake Stream, MaineLargest measured flow of each year at Grand Lake Stream at Grand Lake Stream, Maine: Grand Lake Stream at Grand Lake Stream, Maine in m³/s, from 1929 to 2025.Hurricane Katrina water and sanitation collapse0255075100m³/s19291941195419661978199220042017

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
PeriodGrand Lake Stream at Grand Lake Stream, Maine (m³/s)
192946.7
193040.5
193123.4
193241.1
193330.9
193438.5
193540.2
193647.6
193760.9
193822.7
193937.1
194039.1
194126.0
194249.0
194323.6
194433.7
194547.6
194634.0
194751.0
194928.6
195027.2
195153.5
195265.4
195354.4
195456.9
195552.1
195650.4
195718.8
195856.4
195954.4
196057.8
196158.9
196234.8
196349.0
196447.3
196520.8
196615.2
196730.3
196834.5
196934.3
197049.3
197148.1
197234.0
197356.1
197439.6
197528.0
197656.4
197739.1
197835.1
197956.1
198034.3
198132.3
198241.3
198381.3
198470.8
198633.1
198816.4
198970.2
199053.8
199139.1
199237.4
199324.3
199445.3
199516.5
199649.3
199732.0
199845.3
199932.0
200045.3
200113.1
200219.4
200326.6
200442.2
200583.0
200752.1
200868.0
200945.0
201042.5
201139.1
201227.0
201343.0
201445.0
201540.5
201636.5
201747.9
201841.9
201964.6
202027.6
202121.5
202253.8
202458.0
202542.5

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 held1929–2025
Completeness94.8% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 5 separate periods inside 1929–2025 hold no value. 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 95% 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 St. Croix River at Vanceboro, Maine, 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 St. Croix River at Vanceboro, Maine, as a depthWater leaving the catchment above St. Croix River at Vanceboro, Maine, as a depth: St. Croix River at Vanceboro, Maine in mm, from 1929 to 2025.Hurricane Katrina water and sanitation collapse2004006008001,000mm19291942195519681981199420072020

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
PeriodSt. Croix River at Vanceboro, Maine (mm)
1929590
1930528
1931331
1932591
1933558
1934662
1935572
1936746
1937553
1938435
1939639
1940530
1941538
1942532
1943437
1944438
1945786
1946565
1947646
1948379
1949483
1950524
1951827
1952693
1953552
1954888
1955782
1956449
1957379
1958674
1959741
1960761
1961732
1962550
1963772
1964614
1965410
1966446
1967433
1968645
1969569
1970753
1971658
1972479
1973938
1974596
1975418
1976803
1977704
1978719
1979861
1980496
1981900
1982648
1983756
1984911
1985309
1986485
1987349
1988473
1989621
1990652
1991744
1992641
1993484
1994751
1995412
1996828
1997616
1998595
1999490
2000736
2001379
2002429
2003611
2004523
2005860
2006792
2007566
2008814
2009764
2010812
2011857
2012692
2013906
2014989
2015716
2016700
2017604
2018771
2019907
2020637
2021520
2022760
2023846
2024658
2025613

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
Completeness100.0% of the periods in that span are held.
ContinuityContinuous: every year from 1929 to 2025 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

Every gauge Hydrionis holds within this area

Gauges within the Saint Croix River and what each holds
GaugeMeasuresValuesRecord
Grand Lake Stream at Grand Lake Stream, Maineburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3271929–2026
St. Croix River at Vanceboro, Mainecatchment area, annual maximum river flow, mean river flow, mean river flow, water year2901929–2026
ST. CROIX RIVER NEAR BAILEYVILLE, MEburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2271920–2026

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 — 01050001. 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
Grand Lake Stream at Grand Lake Stream, MaineStated 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
St. Croix River at Vanceboro, MaineStated 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
ST. CROIX RIVER NEAR BAILEYVILLE, MEStated 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 spanned107yes, 20 or more
Values held844no
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), Saint Croix River gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-saint-croix-river/

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 Saint Croix River 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 confidence2025-05-11

Source: USGS — National Water Information System, USGS site 01019000, 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.