The monitoring network within this area

Hydrionis holds 556 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
556
Values held
1901–2026
Record spans
Gauges within the Upper Kennebec River huc8 subbasin
2 monitoring points, positioned as the publisher records them.
Gauges within the Upper Kennebec River huc8 subbasinKENNEBEC RIVER AT MOOSEHEAD, ME, Kennebec River at The Forks, MaineKENNEBEC RIVER AT MOOSEHEAD, MEKennebec River at The Forks, Maine

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 Kennebec River at The Forks, Maine
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1901–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at Kennebec River at The Forks, MaineLargest measured flow of each year at Kennebec River at The Forks, Maine: Kennebec River at The Forks, Maine in m³/s, from 1901 to 2025.Hurricane Katrina water and sanitation collapse02505007501,000m³/s19011917193419481966198420022018

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
PeriodKennebec River at The Forks, Maine (m³/s)
1901634
1903326
1904326
1905331
1906337
1907331
1909422
1910289
1911244
1912459
1913385
1914493
1915270
1916303
1917671
1918274
1920413
1921267
1922388
1923501
1924258
1925328
1927328
1928422
1929467
1930246
1932271
1933286
1934246
1935246
1936430
1937402
1938408
1939207
1940230
1941139
1942374
1943289
1944139
1945535
1946394
1947530
1948148
1949112
1950146
1952233
1953365
1954504
1956224
1957235
1958368
1959572
1960377
1961552
1963292
1964265
1966306
1967311
1968311
1969609
1971334
1973473
1975278
1976419
1977320
1978300
1979487
1980283
1981612
1983932
1984858
1985289
1986259
1987578
1989416
1991439
1993311
1994309
1996436
1997357
1998439
1999354
2000555
2001303
2002268
2003331
2005564
2007436
2008510
2009309
2010351
2011547
2012532
2013377
2014399
2015297
2016306
2017447
2018544
2019498
2020323
2021264
2022303
2023428
2025391

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 held1901–2025
Completeness84.0% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 20 separate periods inside 1901–2025 hold no value. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1901 and is not continuous from it: 125 years separate the first value from the last, and 84% 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 Kennebec River at The Forks, 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. 1904–2024.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above Kennebec River at The Forks, Maine, as a depthWater leaving the catchment above Kennebec River at The Forks, Maine, as a depth: Kennebec River at The Forks, Maine in mm, from 1904 to 2024.Hurricane Katrina water and sanitation collapse2004006008001,000mm19041920193619521968198420002016

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
PeriodKennebec River at The Forks, Maine (mm)
1904539
1905491
1906518
1907654
1908652
1909536
1910567
1911329
1912579
1913590
1914561
1915391
1916537
1917847
1918569
1919690
1920648
1921529
1922522
1923482
1924483
1925525
1926495
1927523
1928667
1929608
1930523
1931382
1932484
1933551
1934452
1935529
1936670
1937580
1938610
1939512
1940478
1941394
1942448
1943500
1944442
1945650
1946553
1947679
1948369
1949382
1950410
1951666
1952532
1953557
1954858
1955640
1956473
1957389
1958676
1959568
1960619
1961640
1962449
1963692
1964467
1965339
1966479
1967528
1968507
1969749
1970751
1971548
1972518
1973912
1974817
1975528
1976743
1977667
1978711
1979600
1980377
1981580
1982624
1983703
1984771
1985451
1986613
1987495
1988458
1989517
1990694
1991652
1992525
1993564
1994594
1995536
1996960
1997589
1998713
1999568
2000697
2001423
2002378
2003508
2004548
2005885
2006770
2007736
2008902
2009747
2010746
2011884
2012632
2013640
2014621
2015556
2016508
2017700
2018574
2019709
2020508
2021370
2022616
2023866
2024525

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 held1904–2024
Completeness100.0% of the periods in that span are held.
ContinuityContinuous: every year from 1904 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

Every gauge Hydrionis holds within this area

Gauges within the Upper Kennebec River and what each holds
GaugeMeasuresValuesRecord
Kennebec River at The Forks, Mainecatchment area, annual maximum river flow, mean river flow, mean river flow, water year3671901–2026
KENNEBEC RIVER AT MOOSEHEAD, MEcatchment area, annual maximum river flow, mean river flow, mean river flow, water year1891919–2026

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 — 01030001. 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
Kennebec River at The Forks, 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
KENNEBEC RIVER AT MOOSEHEAD, 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 2 of them, which makes it a profile, not indexed.

Information-gain signals held for this water body
SignalHeldCounts
Gauges holding a real record2no
Years spanned126yes, 20 or more
Values held556no
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), Upper Kennebec River gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-upper-kennebec-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 Upper Kennebec 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 confidence2025-06-01

Source: USGS — National Water Information System, USGS site 01042500, 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.