The monitoring network within this area

Hydrionis holds 1,344 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
1,344
Values held
1911–2026
Record spans
Gauges within the St. Joe huc8 subbasin
2 monitoring points, positioned as the publisher records them.
Gauges within the St. Joe huc8 subbasinST JOE RIVER AT CALDER, ID, ST MARIES RIVER AT LOTUS IDST JOE RIVER AT CALDER, IDST MARIES RIVER AT LOTUS 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 ST JOE RIVER AT CALDER, ID
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1911–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at ST JOE RIVER AT CALDER, IDLargest measured flow of each year at ST JOE RIVER AT CALDER, ID: ST JOE RIVER AT CALDER, ID in m³/s, from 1911 to 2025.Hurricane Katrina water and sanitation collapse05001,0001,5002,000m³/s19111932194819611976199220062020

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
PeriodST JOE RIVER AT CALDER, ID (m³/s)
1911408
1912445
1921493
1922498
1923385
1924371
1925487
1926326
1927510
1928470
1929265
1930241
1931249
1932493
1933555
1935379
1936566
1937360
19381,303
1939391
1940230
1941150
1943419
1944155
1945439
1946430
1948671
1949544
1950521
1951487
1952459
1953385
1954578
1955515
1956583
1957473
1958396
1959430
1960382
1961439
1962470
1964541
1966408
1967515
1968396
1969470
1970416
1971651
1972612
1973184
1974934
1975470
1976612
1977191
1979595
1980362
1982674
1983360
1984408
1985405
1986419
1987377
1988360
1989402
1990680
1992198
1993394
1994254
1995595
19961,110
1997711
1998264
1999473
2000436
2001227
2002668
2003513
2004270
2006388
2008654
2009388
2010221
2011646
2012586
2013396
2014479
2015388
2016289
2017640
2018566
2019371
2020351
2021261
2022481
2023479
2024180
2025281

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 held1911–2025
Completeness84.3% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 11 separate periods inside 1911–2025 hold no value. The longest runs from 1913 to 1920 — 8 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1911 and is not continuous from it: 115 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 ST JOE RIVER AT CALDER, 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. 1921–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above ST JOE RIVER AT CALDER, ID, as a depthWater leaving the catchment above ST JOE RIVER AT CALDER, ID, as a depth: ST JOE RIVER AT CALDER, ID in mm, from 1921 to 2025.Hurricane Katrina water and sanitation collapse2505007501,0001,250mm19211935194919631977199120052019

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
PeriodST JOE RIVER AT CALDER, ID (mm)
19211,024
1922662
1923764
1924624
19251,023
1926602
19271,185
1928870
1929459
1930492
1931456
1932941
19331,216
1934970
1935729
1936691
1937548
1938807
1939596
1940582
1941486
1942574
1943877
1944342
1945633
1946897
1947859
1948997
1949800
19501,212
1951847
1952671
1953730
1954946
1955874
19561,059
1957809
1958793
19591,064
1960757
1961862
1962836
1963606
1964888
1965907
1966641
1967786
1968780
1969836
1970773
19711,072
19721,173
1973464
19741,262
1975847
1976878
1977507
1978745
1979684
1980764
1981734
1982976
1983815
1984779
1985795
1986733
1987494
1988511
1989792
1990973
1991892
1992479
1993638
1994434
1995985
1996986
19971,244
1998623
1999884
2000747
2001396
2002927
2003643
2004685
2005564
2006841
2007653
2008881
2009727
2010527
20111,138
2012967
2013622
2014850
2015542
2016711
2017993
2018885
2019559
2020680
2021566
2022820
2023530
2024512
2025691

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 held1921–2025
Completeness100.0% of the periods in that span are held.
ContinuityContinuous: every year from 1921 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

The snow standing above this water

2 automated snow stations sit inside this drainage area, weighing the snowpack rather than measuring how deep it is.

483
Fullest snowpack recorded at Sherwin, in 1997 (mm of water)
59
Thinnest, in 2026 (mm of water)
February
Month the pack is usually at its fullest
May
Month the pack has gone by, in half of years
Peak snowpack at Sherwin
Water years 1983–2026. Each point is the fullest month of that snow season.
Peak snowpack at SherwinPeak snowpack at Sherwin: Sherwin in mm, from 1983 to 2026.0200400mm19831989199520022008201420202026Sherwin 1983: 192 mmSherwin 1984: 258 mmSherwin 1985: 387 mmSherwin 1986: 228 mmSherwin 1987: 162 mmSherwin 1988: 179 mmSherwin 1989: 416 mmSherwin 1990: 304 mmSherwin 1991: 183 mmSherwin 1992: 137 mmSherwin 1993: 250 mmSherwin 1994: 191 mmSherwin 1995: 214 mmSherwin 1996: 178 mmSherwin 1997: 483 mmSherwin 1998: 187 mmSherwin 2000: 326 mmSherwin 2001: 221 mmSherwin 2002: 451 mmSherwin 2003: 97.0 mmSherwin 2004: 277 mmSherwin 2005: 63.0 mmSherwin 2006: 218 mmSherwin 2007: 236 mmSherwin 2008: 401 mmSherwin 2009: 252 mmSherwin 2010: 100 mmSherwin 2011: 325 mmSherwin 2012: 299 mmSherwin 2013: 161 mmSherwin 2014: 188 mmSherwin 2015: 90.0 mmSherwin 2016: 181 mmSherwin 2017: 233 mmSherwin 2018: 248 mmSherwin 2019: 241 mmSherwin 2020: 252 mmSherwin 2021: 256 mmSherwin 2022: 244 mmSherwin 2023: 298 mmSherwin 2024: 113 mmSherwin 2025: 137 mmSherwin 2026: 59.0 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
PeriodSherwin (mm)
1983192
1984258
1985387
1986228
1987162
1988179
1989416
1990304
1991183
1992137
1993250
1994191
1995214
1996178
1997483
1998187
2000326
2001221
2002451
200397.0
2004277
200563.0
2006218
2007236
2008401
2009252
2010100
2011325
2012299
2013161
2014188
201590.0
2016181
2017233
2018248
2019241
2020252
2021256
2022244
2023298
2024113
2025137
202659.0

Read against the river

Sherwin and ST JOE RIVER AT CALDER, ID both sit in this drainage area, and their records overlap by 42 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 St. Joe and what each holds
GaugeMeasuresValuesRecord
ST JOE RIVER AT CALDER, IDburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3531911–2026
ST MARIES RIVER AT LOTUS IDcatchment area, annual maximum river flow291921–2026

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 — 17010304. 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
ST JOE RIVER AT CALDER, 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
ST MARIES RIVER AT LOTUS 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 4 of them, which makes it a full profile.

Information-gain signals held for this water body
SignalHeldCounts
Gauges holding a real record1no
Years spanned116yes, 20 or more
Values held1,344yes, 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), St. Joe gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-st-joe/

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 St. Joe 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 confidence2025-03-28

Source: USGS — National Water Information System, USGS site 12414500, 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.