The monitoring network within this area

Hydrionis holds 887 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
887
Values held
1912–2026
Record spans
Gauges within the Waits River-Connecticut River huc8 subbasin
3 monitoring points, positioned as the publisher records them.
Gauges within the Waits River-Connecticut River huc8 subbasinCONNECTICUT RIVER AT WEST LEBANON, NH, MASCOMA RIVER AT MASCOMA, NH, SUGAR RIVER AT WEST CLAREMONT, NHCONNECTICUT RIVER AT WEST LEBANON, NHMASCOMA RIVER AT MASCOMA, NHSUGAR RIVER AT WEST CLAREMONT, 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 AT WEST LEBANON, NH
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1912–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at CONNECTICUT RIVER AT WEST LEBANON, NHLargest measured flow of each year at CONNECTICUT RIVER AT WEST LEBANON, NH: CONNECTICUT RIVER AT WEST LEBANON, NH in m³/s, from 1912 to 2025.Hurricane Katrina water and sanitation collapse01,0002,0003,0004,000m³/s19121925193919541967198319982012

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
PeriodCONNECTICUT RIVER AT WEST LEBANON, NH (m³/s)
19121,977
19133,200
19141,948
19151,257
19161,184
19171,133
19181,371
19191,676
19201,371
19211,147
19222,534
19231,869
19241,184
19251,948
19261,651
1927977
19291,116
1930937
1931852
19321,470
19331,945
19341,620
1935940
19363,398
19371,458
19382,333
19391,495
19401,688
1941906
19421,119
19431,059
19441,042
19451,215
19471,795
19481,073
19501,220
19511,184
19521,600
19532,076
19541,436
19551,427
19561,158
1957651
19581,625
19591,045
19601,614
19611,045
19621,277
19631,116
19641,237
1965617
1966835
19671,274
19681,322
19691,756
19701,334
19711,283
19721,756
19732,240
19751,189
19761,994
19791,388
1980900
19811,348
19821,614
19831,291
19841,872
1985631
19861,430
19871,937
19881,186
19891,328
19901,252
19921,311
19931,212
19941,659
1995807
19961,424
19981,696
1999900
20001,342
20011,674
20021,841
20031,158
20051,461
20061,254
20071,099
20081,385
20091,096
20101,254
20112,973
2012793
20131,051
20141,705
20151,133
20161,297
20171,546
20181,045
20191,849
20201,042
2021915
2022694
20231,948
20251,093

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 held1912–2025
Completeness91.2% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 9 separate periods inside 1912–2025 hold no value. The longest runs from 1977 to 1978 — 2 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1912 and is not continuous from it: 114 years separate the first value from the last, and 91% 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 WEST LEBANON, 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. 1913–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above CONNECTICUT RIVER AT WEST LEBANON, NH, as a depthWater leaving the catchment above CONNECTICUT RIVER AT WEST LEBANON, NH, as a depth: CONNECTICUT RIVER AT WEST LEBANON, NH in mm, from 1913 to 2025.Hurricane Katrina water and sanitation collapse2004006008001,000mm19131933194619591972198820012014

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 WEST LEBANON, NH (mm)
1913667
1919622
1922669
1923614
1924627
1925715
1926628
1927699
1928683
1929590
1930502
1931460
1932590
1933542
1934545
1935544
1936738
1937680
1938650
1939580
1940572
1941393
1942541
1943676
1944516
1945816
1946607
1947668
1948492
1949465
1950565
1951599
1952595
1953577
1954842
1955564
1956549
1957485
1958619
1959629
1960578
1961480
1962559
1963496
1964462
1965395
1966510
1967517
1968519
1969720
1970552
1971506
1972657
1973921
1974754
1975612
1979616
1980440
1981733
1982581
1983755
1984662
1985513
1986610
1987539
1988464
1989590
1990847
1991598
1992519
1993533
1994583
1995493
1996892
1997607
1998709
1999537
2000664
2001437
2002602
2003672
2004561
2005823
2006864
2007661
2008907
2009769
2010719
2011861
2012541
2013656
2014659
2015595
2016532
2017714
2018644
2019777
2020548
2021452
2022556
2023848
2024724
2025552

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 held1913–2025
Completeness91.2% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 3 separate periods inside 1913–2025 hold no value. The longest runs from 1914 to 1918 — 5 years with no reading. 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 91% 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 Waits River-Connecticut River and what each holds
GaugeMeasuresValuesRecord
SUGAR RIVER AT WEST CLAREMONT, NHburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3281928–2026
CONNECTICUT RIVER AT WEST LEBANON, NHcatchment area, annual maximum river flow, mean river flow, mean river flow, water year3191912–2026
MASCOMA RIVER AT MASCOMA, NHcatchment area, annual maximum river flow, mean river flow, mean river flow, water year2401923–2026

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 — 01080104. 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
SUGAR RIVER AT WEST CLAREMONT, 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/42026-10-02
CONNECTICUT RIVER AT WEST LEBANON, 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/42026-10-02
MASCOMA RIVER AT MASCOMA, 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/42026-10-02

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 spanned115yes, 20 or more
Values held887no
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), Waits River-Connecticut River gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-waits-river-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 Waits River-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 confidence2025-05-10

Source: USGS — National Water Information System, USGS site 01152500, 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.