The monitoring network within this area

Hydrionis holds 1,456 values from 5 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.

5
Gauges
1,456
Values held
1891–2026
Record spans
Gauges within the Lower Kennebec River huc8 subbasin
5 monitoring points, positioned as the publisher records them.
Gauges within the Lower Kennebec River huc8 subbasinKennebec River at Bingham, Maine, Carrabassett River near North Anson, Maine, Sandy River near Mercer, Maine, Sebasticook River near Pittsfield, Maine, Cobbosseecontee Stream at Gardiner, MaineKennebec River at Bingham, MaineCarrabassett River near North Anson, MaineSandy River near Mercer, MaineSebasticook River near Pittsfield, MaineCobbosseecontee Stream at Gardiner, 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 Cobbosseecontee Stream at Gardiner, Maine
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1891–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at Cobbosseecontee Stream at Gardiner, MaineLargest measured flow of each year at Cobbosseecontee Stream at Gardiner, Maine: Cobbosseecontee Stream at Gardiner, Maine in m³/s, from 1891 to 2025.Hurricane Katrina water and sanitation collapse050100150m³/s18911907192319381953198219972013

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
PeriodCobbosseecontee Stream at Gardiner, Maine (m³/s)
189180.1
18929.51
189383.3
189428.9
189581.6
189683.8
189728.3
189839.1
189944.5
190075.0
190199.4
1903102
190485.5
190527.4
190639.6
190752.7
190856.6
190962.3
191027.4
191123.8
191249.3
191351.8
191449.0
191529.7
191665.7
1917120
191835.7
191981.8
1920111
1922132
192394.9
192471.4
192562.9
192666.5
192753.5
192879.6
192992.0
193075.3
193161.4
193290.0
193377.6
193483.8
193567.7
1936142
193764.6
193858.9
193979.9
194080.4
19419.00
194237.9
194358.9
194455.2
194566.5
194637.4
194754.9
194890.6
194937.4
195056.9
195186.1
195276.7
195382.7
195479.0
195674.8
19578.55
195868.5
195955.5
196090.0
196174.2
196246.4
196470.8
1977101
197853.5
197962.3
198050.4
198127.5
198246.4
198399.4
1984101
198551.0
198661.4
1987120
198852.1
198981.8
199053.8
199164.0
199263.1
199377.6
199453.0
199531.4
199662.3
199755.2
199879.0
199949.3
200055.8
200160.6
200237.1
200335.4
2005110
200665.4
200780.7
200849.6
200959.5
201069.9
201164.0
201276.2
201335.1
201447.3
201547.9
201751.3
201839.1
201942.2
202054.9
202234.3
202358.9
202460.0
202535.4

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 held1891–2025
Completeness85.9% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 8 separate periods inside 1891–2025 hold no value. The longest runs from 1965 to 1976 — 12 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1891 and is not continuous from it: 135 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 Cobbosseecontee Stream at Gardiner, 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. 1906–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above Cobbosseecontee Stream at Gardiner, Maine, as a depthWater leaving the catchment above Cobbosseecontee Stream at Gardiner, Maine, as a depth: Cobbosseecontee Stream at Gardiner, Maine in mm, from 1906 to 2025.Hurricane Katrina water and sanitation collapse2505007501,000mm19061920193419481962198920032017

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
PeriodCobbosseecontee Stream at Gardiner, Maine (mm)
1906518
1907475
1908510
1909476
1910372
1911295
1912475
1913456
1914538
1915355
1916573
1917754
1918440
1919523
1920956
1921481
1922576
1923530
1924472
1925370
1926499
1927502
1928629
1929608
1930457
1931440
1932418
1933528
1934508
1935572
1936743
1937654
1938548
1939502
1940582
1941262
1942432
1943505
1944545
1945704
1946476
1947508
1948400
1949447
1950426
1951843
1952715
1953729
1954878
1955479
1956593
1957337
1958788
1959607
1960851
1961618
1962598
1963681
1977873
1978554
1979775
1980396
1981531
1982461
19831,010
1984896
1985307
1986602
1987549
1988329
1989558
1990711
1991663
1992494
1993534
1994559
1995502
1996881
1997491
1998717
1999633
2000610
2001399
2002451
2003551
2004436
20051,052
2006875
2007629
2008956
2009915
2010793
2011746
2012580
2013657
2014716
2015533
2016488
2017561
2018617
2019767
2020641
2021510
2022648
2023940
2024728
2025413

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 held1906–2025
Completeness89.2% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • One period inside 1906–2025 holds no value: 1964 to 1976, 13 years with no reading. It is drawn as a break in the line and is never interpolated across.
ContinuityThe record begins in 1906 and is not continuous from it: 120 years separate the first value from the last, and 89% 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 Lower Kennebec River and what each holds
GaugeMeasuresValuesRecord
Cobbosseecontee Stream at Gardiner, Mainecatchment area, annual maximum river flow, mean river flow, mean river flow, water year3391891–2026
Carrabassett River near North Anson, Mainecatchment area, annual maximum river flow, mean river flow, mean river flow, water year3081902–2026
Kennebec River at Bingham, Mainecatchment area, annual maximum river flow, mean river flow, mean river flow, water year2891907–2026
Sandy River near Mercer, Mainecatchment area, annual maximum river flow, mean river flow, mean river flow, water year2661929–2026
Sebasticook River near Pittsfield, Mainecatchment area, annual maximum river flow, mean river flow, mean river flow, water year2541929–2026

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 — 01030003. 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
Cobbosseecontee Stream at Gardiner, 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
Carrabassett River near North Anson, 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 Bingham, 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
Sandy River near Mercer, 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
Sebasticook River near Pittsfield, 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

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 record5yes, 3 or more
Years spanned136yes, 20 or more
Values held1,456yes, 1000 or more
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), Lower Kennebec River gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-lower-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 Lower 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 confidence2025-05-11

Source: USGS — National Water Information System, USGS site 01049500, 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.