The monitoring network within this area

Hydrionis holds 941 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
941
Values held
1919–2026
Record spans
Gauges within the Outlet Connecticut River huc8 subbasin
3 monitoring points, positioned as the publisher records them.
Gauges within the Outlet Connecticut River huc8 subbasinCONNECTICUT RIVER AT THOMPSONVILLE, CT, HOCKANUM RIVER NEAR EAST HARTFORD, CT, SALMON RIVER NEAR EAST HAMPTON, CTCONNECTICUT RIVER AT THOMPSONVILLE, CTHOCKANUM RIVER NEAR EAST HARTFORD, CTSALMON RIVER NEAR EAST HAMPTON, CT

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 HOCKANUM RIVER NEAR EAST HARTFORD, CT
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1920–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at HOCKANUM RIVER NEAR EAST HARTFORD, CTLargest measured flow of each year at HOCKANUM RIVER NEAR EAST HARTFORD, CT: HOCKANUM RIVER NEAR EAST HARTFORD, CT in m³/s, from 1920 to 2025.Hurricane Katrina water and sanitation collapse050100150m³/s19201940195419661978198920022019

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
PeriodHOCKANUM RIVER NEAR EAST HARTFORD, CT (m³/s)
192052.7
192933.7
193011.0
193111.5
193212.3
193314.5
193454.4
193522.9
193651.3
1938146
193937.9
194039.9
194147.9
194218.0
194428.9
194527.2
194710.4
194824.9
195019.8
195128.3
195226.6
195332.6
195432.6
195577.6
195712.9
195815.9
195936.0
196035.1
196125.8
196240.2
196328.3
196417.8
196520.0
196614.2
196723.0
196820.8
196924.9
197057.2
197112.6
197232.6
197351.0
197549.0
197654.1
197735.1
197865.7
197996.3
198049.3
198120.5
198275.9
198356.4
198458.6
198521.7
198623.7
198736.0
198813.7
198927.5
199143.0
199223.4
199323.2
199432.3
199518.4
199657.5
199839.6
199936.5
200039.4
200133.4
200218.0
200436.8
200527.6
200745.9
200844.7
201050.4
201163.7
201345.6
201441.1
201634.8
201734.0
201952.1
202190.3
202229.7
202347.6
202527.3

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 held1920–2025
Completeness77.4% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 17 separate periods inside 1920–2025 hold no value. The longest runs from 1921 to 1928 — 8 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1920 and is not continuous from it: 106 years separate the first value from the last, and 77% 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 CONNECTICUT RIVER AT THOMPSONVILLE, CT, 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 CONNECTICUT RIVER AT THOMPSONVILLE, CT, as a depthWater leaving the catchment above CONNECTICUT RIVER AT THOMPSONVILLE, CT, as a depth: CONNECTICUT RIVER AT THOMPSONVILLE, CT 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
PeriodCONNECTICUT RIVER AT THOMPSONVILLE, CT (mm)
1929568
1930437
1931467
1932545
1933588
1934585
1935546
1936715
1937712
1938756
1939550
1940578
1941346
1942525
1943644
1944475
1945752
1946522
1947602
1948524
1949459
1950539
1951684
1952661
1953661
1954746
1955707
1956598
1957449
1958605
1959618
1960667
1961508
1962510
1963438
1964425
1965315
1966422
1967524
1968529
1969708
1970552
1971476
1972708
1973823
1974657
1975695
1976809
1977713
1978556
1979771
1980455
1981595
1982561
1983784
1984748
1985450
1986666
1987638
1988511
1989677
1990855
1991622
1992545
1993614
1994642
1995516
1996929
1997613
1998673
1999557
2000700
2001495
2002537
2003748
2004562
2005828
2006841
2007631
2008914
2009747
2010689
2011963
2012499
2013640
2014696
2015540
2016473
2017663
2018783
2019742
2020555
2021633
2022533
2023880
2024658
2025543

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 Outlet Connecticut River and what each holds
GaugeMeasuresValuesRecord
SALMON RIVER NEAR EAST HAMPTON, CTburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3281928–2026
CONNECTICUT RIVER AT THOMPSONVILLE, CTburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3271928–2026
HOCKANUM RIVER NEAR EAST HARTFORD, CTcatchment area, annual maximum river flow, mean river flow, mean river flow, water year2861919–2026

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 — 01080205. 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
SALMON RIVER NEAR EAST HAMPTON, CTStated 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
CONNECTICUT RIVER AT THOMPSONVILLE, CTStated 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
HOCKANUM RIVER NEAR EAST HARTFORD, CTStated 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 spanned108yes, 20 or more
Values held941no
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), Outlet Connecticut River gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-outlet-connecticut-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 Outlet Connecticut 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 confidence2025-05-09

Source: USGS — National Water Information System, USGS site 01193500, 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.