The monitoring network within this area

Hydrionis holds 1,841 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
1,841
Values held
1909–2026
Record spans
Gauges within the Lower Henrys huc8 subbasin
5 monitoring points, positioned as the publisher records them.
Gauges within the Lower Henrys huc8 subbasinHENRYS FORK NR ASHTON ID, FALL RIVER NR CHESTER ID, HENRYS FORK AT ST ANTHONY ID, HENRYS FORK NR REXBURG ID, FALL RIVER NR SQUIRREL IDHENRYS FORK NR ASHTON IDFALL RIVER NR CHESTER IDHENRYS FORK AT ST ANTHONY IDHENRYS FORK NR REXBURG IDFALL RIVER NR SQUIRREL ID

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 FALL RIVER NR CHESTER ID
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 FALL RIVER NR CHESTER IDLargest measured flow of each year at FALL RIVER NR CHESTER ID: FALL RIVER NR CHESTER ID in m³/s, from 1920 to 2025.Hurricane Katrina water and sanitation collapse0100200300m³/s19201933194819611974198820022015

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
PeriodFALL RIVER NR CHESTER ID (m³/s)
192092.3
1921105
192292.6
192375.3
192443.9
1925121
192666.0
1927181
1928128
1929106
193099.1
193186.1
1932161
1933119
193437.1
193574.5
1936106
193774.2
194096.8
194172.2
194279.9
194387.2
194473.9
194587.8
194671.6
194798.0
1948117
1949114
195095.1
195185.8
1952108
195388.3
195497.4
195569.7
195698.8
1957111
195895.1
195992.0
1960125
196166.3
196288.3
196387.2
1964123
196596.3
196677.3
1967123
1968130
196978.7
1970162
1971121
1972106
1973120
1974179
1975163
1976149
197766.0
1978139
1979102
198087.5
1981219
1982113
1983140
1984149
1985107
1986108
198862.3
1989122
199069.4
1991118
199271.6
1993137
1994106
1995104
1996163
1997153
1998109
1999135
200097.1
2002106
200396.8
200471.1
200584.7
2006117
200774.8
2008147
200998.8
2010218
2011264
2012106
201375.6
2014104
201560.6
201668.5
2017110
2018108
2019111
202098.8
202184.4
2022131
2023115
202473.9
202572.2

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
Completeness96.2% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 3 separate periods inside 1920–2025 hold no value. The longest runs from 1938 to 1939 — 2 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 96% 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 HENRYS FORK NR REXBURG ID, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1910–2024.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above HENRYS FORK NR REXBURG ID, as a depthWater leaving the catchment above HENRYS FORK NR REXBURG ID, as a depth: HENRYS FORK NR REXBURG ID in mm, from 1910 to 2024.Hurricane Katrina water and sanitation collapse0200400mm19101925194019551970198520002015

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
PeriodHENRYS FORK NR REXBURG ID (mm)
1910257
1911284
1912322
1913333
1914300
1915207
1916272
1917322
1918265
1919194
1920204
1921266
1922227
1923204
1924120
1925305
1926176
1927311
1928264
1929213
1930151
1931101
1932200
1933176
193482.0
1935138
1936186
1937152
1938231
1939181
1940187
1941163
1942181
1943284
1944212
1945256
1946242
1947218
1948248
1949246
1950263
1951270
1952294
1953219
1954206
1955204
1956256
1957275
1958207
1959188
1960168
1961156
1962235
1963207
1964254
1965293
1966176
1967242
1968258
1969279
1970308
1971391
1972366
1973275
1974356
1975353
1976376
1977152
1978256
1979232
1980247
1981228
1982356
1983412
1984479
1985306
1986390
1987186
1988178
1989244
1990184
1991211
1992161
1993289
1994182
1995348
1996338
1997492
1998374
1999377
2000235
2001169
2002194
2003175
2004200
2005211
2006296
2007206
2008268
2009259
2010209
2011386
2012252
2013197
2014230
2015178
2016176
2017305
2018281
2019271
2020231
2021171
2022169
2023246
2024212

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 held1910–2024
Completeness100.0% of the periods in that span are held.
ContinuityContinuous: every year from 1910 to 2024 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

The snow standing above this water

1 automated snow station sits inside this drainage area, weighing the snowpack rather than measuring how deep it is.

1,439
Fullest snowpack recorded at Grassy Lake, in 1982 (mm of water)
424
Thinnest, in 2026 (mm of water)
April
Month the pack is usually at its fullest
June
Month the pack has gone by, in half of years
Peak snowpack at Grassy Lake
Water years 1981–2026. Each point is the fullest month of that snow season.
Peak snowpack at Grassy LakePeak snowpack at Grassy Lake: Grassy Lake in mm, from 1981 to 2026.05001,0001,500mm19811987199319992005201120172023Grassy Lake 1981: 575 mmGrassy Lake 1982: 1,439 mmGrassy Lake 1983: 1,026 mmGrassy Lake 1984: 857 mmGrassy Lake 1985: 755 mmGrassy Lake 1986: 1,022 mmGrassy Lake 1987: 444 mmGrassy Lake 1988: 678 mmGrassy Lake 1989: 988 mmGrassy Lake 1990: 683 mmGrassy Lake 1991: 779 mmGrassy Lake 1992: 560 mmGrassy Lake 1993: 899 mmGrassy Lake 1994: 614 mmGrassy Lake 1995: 979 mmGrassy Lake 1996: 967 mmGrassy Lake 1997: 1,211 mmGrassy Lake 1998: 807 mmGrassy Lake 1999: 1,097 mmGrassy Lake 2000: 761 mmGrassy Lake 2001: 556 mmGrassy Lake 2002: 695 mmGrassy Lake 2003: 792 mmGrassy Lake 2004: 879 mmGrassy Lake 2005: 603 mmGrassy Lake 2006: 999 mmGrassy Lake 2007: 649 mmGrassy Lake 2008: 990 mmGrassy Lake 2009: 837 mmGrassy Lake 2010: 547 mmGrassy Lake 2011: 1,156 mmGrassy Lake 2012: 790 mmGrassy Lake 2013: 702 mmGrassy Lake 2014: 1,043 mmGrassy Lake 2015: 626 mmGrassy Lake 2016: 691 mmGrassy Lake 2017: 953 mmGrassy Lake 2018: 828 mmGrassy Lake 2019: 857 mmGrassy Lake 2020: 850 mmGrassy Lake 2021: 684 mmGrassy Lake 2022: 581 mmGrassy Lake 2023: 930 mmGrassy Lake 2024: 680 mmGrassy Lake 2025: 741 mmGrassy Lake 2026: 424 mm

A water year runs October to September and is named for the year it ends, so the snow of one winter stays in one point. The value is the fullest month, not the fullest day: a pack that peaked sharply mid-month reads lower here than a single measurement taken at the right moment would.

View the data behind this chart
Underlying data
PeriodGrassy Lake (mm)
1981575
19821,439
19831,026
1984857
1985755
19861,022
1987444
1988678
1989988
1990683
1991779
1992560
1993899
1994614
1995979
1996967
19971,211
1998807
19991,097
2000761
2001556
2002695
2003792
2004879
2005603
2006999
2007649
2008990
2009837
2010547
20111,156
2012790
2013702
20141,043
2015626
2016691
2017953
2018828
2019857
2020850
2021684
2022581
2023930
2024680
2025741
2026424

Read against the river

Grassy Lake and HENRYS FORK NR ASHTON ID both sit in this drainage area, and their records overlap by 44 years. That is the span the two have in common, not a count of years both actually hold — either record may have gaps inside it. The two are shown separately rather than on one axis: millimetres of stored water and cubic metres per second are not commensurable, and a difference between them would mean nothing.

Being in the same drainage area does not put the snowpack upstream of the gauge. A subbasin is an area, and snow on one tributary can join the river below a gauge on another — so a weak relationship here may say more about which tributary was measured than about the snow.

Every gauge Hydrionis holds within this area

Gauges within the Lower Henrys and what each holds
GaugeMeasuresValuesRecord
HENRYS FORK NR REXBURG IDburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3671909–2026
HENRYS FORK NR ASHTON IDburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3261921–2026
FALL RIVER NR CHESTER IDburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2641920–2026
HENRYS FORK AT ST ANTHONY IDburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2611923–2026
FALL RIVER NR SQUIRREL IDcatchment area, annual maximum river flow731949–2026

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 — 17040203. 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
HENRYS FORK NR REXBURG IDStated 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
HENRYS FORK NR ASHTON IDStated 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
FALL RIVER NR CHESTER IDStated 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
HENRYS FORK AT ST ANTHONY IDStated 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
FALL RIVER NR SQUIRREL IDStated 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 spanned118yes, 20 or more
Values held1,841yes, 1000 or more
Distinct measurements6yes, 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), Lower Henrys gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-lower-henrys/

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 Lower Henrys 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 confidence2025-05-14

Source: USGS — National Water Information System, USGS site 13056500, 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.