The monitoring network within this area

Hydrionis holds 1,037 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
1,037
Values held
1909–2026
Record spans
Gauges within the Westfield River huc8 subbasin
3 monitoring points, positioned as the publisher records them.
Gauges within the Westfield River huc8 subbasinWESTFIELD RIVER AT KNIGHTVILLE, MA, MIDDLE BRANCH WESTFIELD RIVER AT GOSS HEIGHTS, MA, WESTFIELD RIVER NEAR WESTFIELD, MAWESTFIELD RIVER AT KNIGHTVILLE, MAMIDDLE BRANCH WESTFIELD RIVER AT GOSS HEIGHTS, MAWESTFIELD RIVER NEAR WESTFIELD, 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 WESTFIELD RIVER AT KNIGHTVILLE, MA
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1910–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at WESTFIELD RIVER AT KNIGHTVILLE, MALargest measured flow of each year at WESTFIELD RIVER AT KNIGHTVILLE, MA: WESTFIELD RIVER AT KNIGHTVILLE, MA in m³/s, from 1910 to 2025.Hurricane Katrina water and sanitation collapse05001,000m³/s19101924193819521965198120002016

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
PeriodWESTFIELD RIVER AT KNIGHTVILLE, MA (m³/s)
1910230
191167.4
1912206
1913194
1914161
1915234
1916112
191791.5
191860.6
1919204
1920191
1922162
1923127
1924297
1925230
1926162
1927138
1929146
193086.4
1931253
1932131
1933447
1934215
1935139
1936728
1937272
19381,073
1939200
1940194
194199.7
194299.1
194438.2
1945189
194680.4
1947109
1948131
1949152
1950100
1951116
195294.3
1953123
195494.3
1955133
1956124
195758.9
1958110
195980.7
1960101
1961117
1962117
196370.8
196473.1
196574.8
196637.9
196767.7
196889.5
1969101
197170.8
197293.7
197392.9
1975114
1976103
1977112
197996.8
1980101
1981102
198297.4
1983112
198496.6
198576.5
198683.8
1987150
198868.5
198971.1
1990103
1996101
199892.9
199996.6
2000104
2001101
200257.8
200380.4
200498.0
2005104
2007105
2008107
200985.5
2010105
2011121
2013105
201491.2
201684.4
2017206
201898.3
202080.7
202185.5
202376.7
202561.4

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 held1910–2025
Completeness84.5% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 14 separate periods inside 1910–2025 hold no value. The longest runs from 1991 to 1995 — 5 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1910 and is not continuous from it: 116 years separate the first value from the last, and 84% 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 WESTFIELD RIVER NEAR WESTFIELD, 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. 1915–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above WESTFIELD RIVER NEAR WESTFIELD, MA, as a depthWater leaving the catchment above WESTFIELD RIVER NEAR WESTFIELD, MA, as a depth: WESTFIELD RIVER NEAR WESTFIELD, MA in mm, from 1915 to 2025.Hurricane Katrina water and sanitation collapse2505007501,0001,250mm19151929194319571971198519992013

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
PeriodWESTFIELD RIVER NEAR WESTFIELD, MA (mm)
1915556
1916658
1917567
1918524
1919608
1920832
1921515
1922621
1923634
1924605
1925549
1926536
1927865
1928787
1929597
1930385
1931526
1932528
1933715
1934703
1935495
1936680
1937845
1938914
1939530
1940622
1941362
1942662
1943723
1944468
1945856
1946517
1947610
1948656
1949548
1950564
1951795
1952821
1953779
1954737
19551,129
1956638
1957381
1958655
1959590
1960714
1961578
1962465
1963415
1964412
1965270
1966380
1967551
1968609
1969728
1970559
1971591
19721,004
1973901
1974676
1975952
1976669
1977841
1978627
1979943
1980503
1981414
1982681
1983921
1984860
1985500
1986623
1987675
1988548
1989696
1990814
1991605
1992599
1993712
1994611
1995570
19961,115
1997622
1998706
1999661
2000778
2001565
2002449
2003878
2004642
2005809
2006755
2007604
2008998
2009742
2010724
20111,208
2012495
2013717
2014733
2015505
2016397
2017587
20181,056
2019693
2020579
2021899
2022549
2023992
2024707
2025547

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 held1915–2025
Completeness100.0% of the periods in that span are held.
ContinuityContinuous: every year from 1915 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 Westfield River and what each holds
GaugeMeasuresValuesRecord
WESTFIELD RIVER NEAR WESTFIELD, MAburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3701914–2026
WESTFIELD RIVER AT KNIGHTVILLE, MAburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3671909–2026
MIDDLE BRANCH WESTFIELD RIVER AT GOSS HEIGHTS, MAburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3001910–2026

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 — 01080206. 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
WESTFIELD RIVER NEAR WESTFIELD, 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
WESTFIELD RIVER AT KNIGHTVILLE, 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
MIDDLE BRANCH WESTFIELD RIVER AT GOSS HEIGHTS, 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

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 5 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 spanned118yes, 20 or more
Values held1,037yes, 1000 or more
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), Westfield River gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-westfield-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 Westfield 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 01183500, 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.