The monitoring network within this area

Hydrionis holds 728 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
728
Values held
1913–2026
Record spans
Gauges within the Farmington River huc8 subbasin
3 monitoring points, positioned as the publisher records them.
Gauges within the Farmington River huc8 subbasinNEPAUG R NR NEPAUG, CT., CLEAR BK NR COLLINSVILLE, CT., WEST BRANCH FARMINGTON RIVER NEAR NEW BOSTON, MANEPAUG R NR NEPAUG, CT.CLEAR BK NR COLLINSVILLE, CT.WEST BRANCH FARMINGTON RIVER NEAR NEW BOSTON, MA

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 WEST BRANCH FARMINGTON RIVER NEAR NEW BOSTON, MA
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1913–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at WEST BRANCH FARMINGTON RIVER NEAR NEW BOSTON, MALargest measured flow of each year at WEST BRANCH FARMINGTON RIVER NEAR NEW BOSTON, MA: WEST BRANCH FARMINGTON RIVER NEAR NEW BOSTON, MA in m³/s, from 1913 to 2025.Hurricane Katrina water and sanitation collapse02505007501,000m³/s19131927194119571971198419992014

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
PeriodWEST BRANCH FARMINGTON RIVER NEAR NEW BOSTON, MA (m³/s)
191390.6
191573.6
191753.8
191828.6
191971.9
192067.7
192171.4
192262.3
192351.0
1924112
192558.0
192649.3
192751.5
192973.3
193031.1
193141.1
193256.1
193463.7
193586.6
1936257
193792.9
1938524
193962.9
194064.6
194141.1
194270.8
194373.9
194569.4
194642.5
194752.7
194890.0
195036.0
1952115
195391.7
1954120
1955971
195742.8
195969.1
196094.6
196183.3
196271.1
196340.8
196516.8
196627.6
196745.3
196864.8
1969121
197041.1
197137.9
197273.3
197351.8
197589.5
1976106
197792.9
197892.0
197995.7
1980170
1981134
198266.3
1983113
1984219
1985154
198645.3
1987244
198841.3
1989143
199094.6
199243.9
199373.3
199457.2
1996127
199849.3
1999103
200066.5
200233.7
200365.7
200495.7
200598.3
2007215
200870.5
2009108
201068.8
2011490
201356.4
201445.3
201651.5
201732.8
201892.0
201952.7
2021119
2023115
202547.9

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 held1913–2025
Completeness81.4% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 21 separate periods inside 1913–2025 hold no value. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1913 and is not continuous from it: 113 years separate the first value from the last, and 81% 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 WEST BRANCH FARMINGTON RIVER NEAR NEW BOSTON, MA, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1914–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above WEST BRANCH FARMINGTON RIVER NEAR NEW BOSTON, MA, as a depthWater leaving the catchment above WEST BRANCH FARMINGTON RIVER NEAR NEW BOSTON, MA, as a depth: WEST BRANCH FARMINGTON RIVER NEAR NEW BOSTON, MA in mm, from 1914 to 2025.Hurricane Katrina water and sanitation collapse2505007501,0001,250mm19141928194219561970198419982012

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
PeriodWEST BRANCH FARMINGTON RIVER NEAR NEW BOSTON, MA (mm)
1914582
1915620
1916728
1917538
1918535
1919644
1920921
1921593
1922659
1923696
1924697
1925572
1926693
19271,108
1928906
1929761
1930398
1931517
1932593
1933696
1934751
1935586
1936740
1937835
1938980
1939602
1940616
1941407
1942701
1943714
1944506
1945969
1946526
1947588
1948801
1949551
1950629
1951831
1952768
1953752
1954743
19551,152
1956716
1957394
1958733
1959646
1960783
1961640
1962420
1963480
1964430
1965257
1966458
1967602
1968648
1969829
1970590
1971690
19721,008
1973931
1974742
1975927
1976727
1977901
1978663
19791,002
1980498
1981480
1982713
1983910
1984895
1985506
1986654
1987720
1988611
1989763
1990816
1991565
1992638
1993778
1994736
1995616
19961,245
1997607
1998709
1999715
2000725
2001541
2002487
2003918
2004770
2005846
2006859
2007647
20081,120
2009844
2010791
20111,234
2012508
2013722
2014865
2015551
2016434
2017577
20181,109
2019722
2020590
2021936
2022615
2023975
2024682
2025501

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 held1914–2025
Completeness100.0% of the periods in that span are held.
ContinuityContinuous: every year from 1914 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 Farmington River and what each holds
GaugeMeasuresValuesRecord
WEST BRANCH FARMINGTON RIVER NEAR NEW BOSTON, MAburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3731913–2026
NEPAUG R NR NEPAUG, CT.burned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year1901921–2026
CLEAR BK NR COLLINSVILLE, CT.burned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year1651921–2026

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 — 01080207. 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
WEST BRANCH FARMINGTON RIVER NEAR NEW BOSTON, MAStated 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
NEPAUG R NR NEPAUG, CT.Stated 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
CLEAR BK NR COLLINSVILLE, CT.Stated 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 spanned114yes, 20 or more
Values held728no
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), Farmington River gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-farmington-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 Farmington 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 confidence2025-05-06

Source: USGS — National Water Information System, USGS site 01185500, 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.