The monitoring network within this area

Hydrionis holds 1,232 values from 5 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.

5
Gauges
1,232
Values held
1915–2026
Record spans
Gauges within the Millers River huc8 subbasin
5 monitoring points, positioned as the publisher records them.
Gauges within the Millers River huc8 subbasinTARBELL BROOK NEAR WINCHENDON, MA, MILLERS RIVER NEAR WINCHENDON, MA, PRIEST BROOK NEAR WINCHENDON, MA, MOSS BROOK AT WENDELL DEPOT, MA, MILLERS RIVER AT ERVING, MATARBELL BROOK NEAR WINCHENDON, MAMILLERS RIVER NEAR WINCHENDON, MAPRIEST BROOK NEAR WINCHENDON, MAMOSS BROOK AT WENDELL DEPOT, MAMILLERS RIVER AT ERVING, 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 MILLERS RIVER AT ERVING, MA
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1915–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at MILLERS RIVER AT ERVING, MALargest measured flow of each year at MILLERS RIVER AT ERVING, MA: MILLERS RIVER AT ERVING, MA in m³/s, from 1915 to 2025.Hurricane Katrina water and sanitation collapse02505007501,000m³/s19151927194219541966198119952011

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
PeriodMILLERS RIVER AT ERVING, MA (m³/s)
1915150
1916108
1917136
191887.5
1919107
1920170
1921150
1922137
1923143
1924149
1925110
192687.5
1927112
1929112
193052.1
193185.5
1932136
1933170
1934139
1935125
1936558
1938821
1940198
194152.4
1942135
194373.1
1944138
194596.6
1946115
194772.2
1948161
194972.8
195073.6
1951114
1952110
1953116
195473.3
195589.8
1956129
195756.4
195892.9
1959139
1960142
196171.4
1962120
1963121
196470.8
196539.4
196675.3
196795.1
1968130
1969101
1970115
197180.7
1972114
1973119
1975136
1977160
1978126
1979204
198187.8
1982111
198397.4
1984193
198566.8
1986139
1987138
198866.0
198981.6
1991104
1993107
1994101
199565.4
1996152
1998121
1999163
200081.0
2001128
200262.6
2003106
2005114
2007112
2008127
2010112
2011156
2013117
2014107
201684.7
2017102
2018111
2019112
2021167
202276.7
2023117
202497.7
2025131

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 held1915–2025
Completeness86.5% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 15 separate periods inside 1915–2025 hold no value. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1915 and is not continuous from it: 111 years separate the first value from the last, and 86% 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 MILLERS RIVER AT ERVING, 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. 1916–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above MILLERS RIVER AT ERVING, MA, as a depthWater leaving the catchment above MILLERS RIVER AT ERVING, MA, as a depth: MILLERS RIVER AT ERVING, MA in mm, from 1916 to 2025.Hurricane Katrina water and sanitation collapse2505007501,000mm19161930194419581972198620002014

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
PeriodMILLERS RIVER AT ERVING, MA (mm)
1916714
1917578
1918513
1919585
1920820
1921615
1922762
1923603
1924506
1925488
1926447
1927654
1928699
1929546
1930278
1931416
1932518
1933645
1934675
1935530
1936731
1937700
1938974
1939473
1940603
1941297
1942529
1943589
1944481
1945737
1946540
1947518
1948572
1949403
1950520
1951789
1952608
1953750
1954655
1955689
1956589
1957410
1958556
1959615
1960751
1961502
1962475
1963364
1964363
1965200
1966303
1967576
1968537
1969631
1970587
1971484
1972795
1973846
1974616
1975835
1976634
1977682
1978503
1979920
1980414
1981532
1982710
1983807
1984849
1985358
1986653
1987591
1988482
1989635
1990657
1991708
1992461
1993539
1994601
1995553
19961,020
1997569
1998625
1999559
2000665
2001477
2002378
2003742
2004618
2005972
2006757
2007531
2008981
2009742
2010633
2011979
2012419
2013598
2014803
2015527
2016401
2017664
20181,058
2019694
2020568
2021781
2022570
2023834
2024675
2025536

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 held1916–2025
Completeness100.0% of the periods in that span are held.
ContinuityContinuous: every year from 1916 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 Millers River and what each holds
GaugeMeasuresValuesRecord
MILLERS RIVER AT ERVING, MAburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3681915–2026
MOSS BROOK AT WENDELL DEPOT, MAburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2341916–2026
MILLERS RIVER NEAR WINCHENDON, MAcatchment area, mean river flow, mean river flow, water year2191916–2026
PRIEST BROOK NEAR WINCHENDON, MAcatchment area, mean river flow, mean river flow, water year2121916–2026
TARBELL BROOK NEAR WINCHENDON, MAcatchment area, annual maximum river flow, mean river flow, mean river flow, water year1991916–2026

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 — 01080202. 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
MILLERS RIVER AT ERVING, 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
MOSS BROOK AT WENDELL DEPOT, 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
MILLERS RIVER NEAR WINCHENDON, 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
PRIEST BROOK NEAR WINCHENDON, 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
TARBELL BROOK NEAR WINCHENDON, 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 record5yes, 3 or more
Years spanned112yes, 20 or more
Values held1,232yes, 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), Millers River gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-millers-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 Millers 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 01166500, 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.