The monitoring network within this area

Hydrionis holds 379 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
379
Values held
1917–2026
Record spans
Gauges within the Headwaters Connecticut River huc8 subbasin
2 monitoring points, positioned as the publisher records them.
Gauges within the Headwaters Connecticut River huc8 subbasinCONNECTICUT R AT FIRST CONN LK NR PITTSBURG, NH, CONNECTICUT RIVER NEAR DALTON, NHCONNECTICUT R AT FIRST CONN LK NR PITTSBURG, NHCONNECTICUT RIVER NEAR DALTON, NH

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 CONNECTICUT RIVER NEAR DALTON, NH
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1928–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at CONNECTICUT RIVER NEAR DALTON, NHLargest measured flow of each year at CONNECTICUT RIVER NEAR DALTON, NH: CONNECTICUT RIVER NEAR DALTON, NH in m³/s, from 1928 to 2025.Hurricane Katrina water and sanitation collapse05001,0001,500m³/s19281940195419661978199020022016

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 recordA 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 collapseFlood2005-08-292005-09-30Documented record
Compiled record

Not shown on this chart

  • The 1976 droughtThis 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 droughtThis event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • Yorkshire droughtThis 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 PauloThis 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 ZeroThis event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • European droughtThis 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 NEAR DALTON, NH (m³/s)
19281,254
1929799
1930484
1931450
1932572
19331,014
1934892
1935637
19361,368
1937555
1938555
1939668
1940886
1941547
1942654
1943606
1944578
1945705
1947617
1948476
1949453
1950603
1952518
1953980
1954966
1955767
1956510
1957391
1958810
1959416
1960776
1961518
1962586
1963597
1964691
1965243
1966413
1967436
1968433
1969833
1970680
1971487
1972912
1973589
1974753
1975459
1976640
1977532
1978532
1979558
1980323
1981586
1982708
1983496
1984804
1985343
1986719
1987827
1988481
1989790
19901,096
1991612
1992753
1993490
1994779
1995847
1996861
1997428
19981,189
1999462
2000682
2001915
2002917
2003564
2005513
2007617
2008555
2009422
2010467
2011940
2012442
2013600
20141,002
2015510
2016377
2017589
2018651
20191,056
2020493
2021498
2022379
2023481
2024600
2025677

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 held19282025
Completeness95.9% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 4 separate periods inside 1928–2025 hold no value. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1928 and is not continuous from it: 98 years separate the first value from the last, and 96% of the years between them are held. The span is not the record.
Last read from the publisher2026-08-31
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 NEAR DALTON, NH, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1928–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above CONNECTICUT RIVER NEAR DALTON, NH, as a depthWater leaving the catchment above CONNECTICUT RIVER NEAR DALTON, NH, as a depth: CONNECTICUT RIVER NEAR DALTON, NH in mm, from 1928 to 2025.Hurricane Katrina water and sanitation collapse4006008001,000mm19281941195419671980199320062019

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 recordA 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 collapseFlood2005-08-292005-09-30Documented record
Compiled record

Not shown on this chart

  • The 1976 droughtThis 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 droughtThis event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • Yorkshire droughtThis 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 PauloThis 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 ZeroThis event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • European droughtThis 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 NEAR DALTON, NH (mm)
1928794
1929705
1930633
1931533
1932716
1933673
1934697
1935608
1936834
1937751
1938701
1939650
1940579
1941455
1942592
1943766
1944601
1945803
1946644
1947742
1948543
1949521
1950648
1951607
1952585
1953592
1954977
1955623
1956609
1957597
1958702
1959693
1960597
1961543
1962662
1963619
1964542
1965505
1966563
1967567
1968596
1969841
1970651
1971574
1972673
1973917
1974807
1975607
1976839
1977773
1978622
1979649
1980525
1981710
1982668
1983728
1984660
1985560
1986637
1987536
1988595
1989637
1990857
1991681
1992540
1993603
1994628
1995545
1996915
1997672
1998746
1999641
2000744
2001524
2002715
2003673
2004647
2005902
2006879
2007759
2008938
2009786
2010766
2011854
2012598
2013690
2014724
2015684
2016582
2017749
2018707
2019864
2020627
2021458
2022615
2023804
2024777
2025598

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 held19282025
Completeness100.0% of the periods in that span are held.
ContinuityContinuous: every year from 1928 to 2025 is held.
Last read from the publisher2026-08-24
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 Headwaters Connecticut River and what each holds
GaugeMeasuresValuesRecord
CONNECTICUT RIVER NEAR DALTON, NHburned area within 50 km, catchment area, annual maximum river flow, mean river flow2331928–2026
CONNECTICUT R AT FIRST CONN LK NR PITTSBURG, NHcatchment area, annual maximum river flow, mean river flow1461917–2026

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 — 01080101. 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
CONNECTICUT RIVER NEAR DALTON, NHStated 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/42026-08-26
CONNECTICUT R AT FIRST CONN LK NR PITTSBURG, NHStated 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/42026-08-26

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 3 of them, which makes it a full profile.

Information-gain signals held for this water body
SignalHeldCounts
Gauges holding a real record2no
Years spanned110yes, 20 or more
Values held379no
Distinct measurements4yes, 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), Headwaters Connecticut River gauge records, accessed 2026-09-02, hydrionis.com/waters/united-states-headwaters-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 Headwaters 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 confidence2025-03-19

Source: USGSNational Water Information System, USGS site 01131500, 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 31 August 2026.