The monitoring network within this area

Hydrionis holds 606 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
606
Values held
1913–2026
Record spans
Gauges within the Whitewater huc8 subbasin
2 monitoring points, positioned as the publisher records them.
Gauges within the Whitewater huc8 subbasinWHITEWATER RIVER NEAR ALPINE, IN, WHITEWATER RIVER AT BROOKVILLE, INWHITEWATER RIVER NEAR ALPINE, INWHITEWATER RIVER AT BROOKVILLE, IN

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 WHITEWATER RIVER AT BROOKVILLE, IN
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1913–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at WHITEWATER RIVER AT BROOKVILLE, INLargest measured flow of each year at WHITEWATER RIVER AT BROOKVILLE, IN: WHITEWATER RIVER AT BROOKVILLE, IN in m³/s, from 1913 to 2025.Hurricane Katrina water and sanitation collapse01,0002,000m³/s19131932194619601973198820022017

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
PeriodWHITEWATER RIVER AT BROOKVILLE, IN (m³/s)
19130
19161,136
1917801
1918484
19191,011
19201,294
1924722
1925262
1926612
1927827
19291,960
1930869
1931328
1932699
19331,130
1935515
1936481
19371,478
1938663
1939861
19401,022
194185.8
1942578
19431,472
1944762
19451,045
1946597
19471,093
19481,070
19491,733
19501,280
1951951
19521,733
1953382
1954132
1955343
19571,000
1958810
19592,316
1960578
19611,189
1962750
19631,826
19641,303
1965646
1966391
1967663
19681,637
1969889
19701,073
1971821
1972498
1973496
1974524
19751,025
1976408
1977399
1978600
1979680
1981422
1982838
1983844
1984419
1985515
1986365
1988473
1989790
1990578
1992442
1993360
1994748
1995595
19961,393
1997745
1998844
1999569
2000507
2001496
2002765
2003345
20041,294
20051,136
2006694
2007671
20081,085
2009997
2010629
2011983
2013394
2015351
2016733
2017756
20181,254
20191,218
20201,085
2021824
2022782
2023807
2024399
20251,229

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 held1913–2025
Completeness88.5% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 10 separate periods inside 1913–2025 hold no value. The longest runs from 1921 to 1923 — 3 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 88% 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 WHITEWATER RIVER AT BROOKVILLE, IN, 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 WHITEWATER RIVER AT BROOKVILLE, IN, as a depthWater leaving the catchment above WHITEWATER RIVER AT BROOKVILLE, IN, as a depth: WHITEWATER RIVER AT BROOKVILLE, IN in mm, from 1916 to 2025.Hurricane Katrina water and sanitation collapse0200400600800mm19161936194919621975198820012014

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
PeriodWHITEWATER RIVER AT BROOKVILLE, IN (mm)
1916429
1924450
1925244
1926532
1927493
1928325
1929564
1930325
1931165
1932379
1933492
193489.0
1935152
1936278
1937520
1938453
1939342
1940218
1941108
1942293
1943330
1944233
1945427
1946266
1947452
1948406
1949500
1950770
1951476
1952382
1953223
1954107
1955343
1956304
1957416
1958513
1959397
1960209
1961417
1962299
1963272
1964268
1965275
1966269
1967386
1968463
1969407
1970319
1971290
1972386
1973461
1974364
1975449
1976207
1977292
1978417
1979654
1980397
1981258
1982457
1983309
1984372
1985465
1986392
1987201
1988183
1989470
1990626
1991390
1992298
1993571
1994346
1995340
1996724
1997417
1998422
1999250
2000293
2001462
2002512
2003545
2004430
2005549
2006689
2007491
2008612
2009374
2010423
2011727
2012268
2013390
2014444
2015424
2016424
2017609
2018656
2019648
2020438
2021469
2022418
2023244
2024350
2025420

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
Completeness93.6% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • One period inside 1916–2025 holds no value: 1917 to 1923, 7 years with no reading. It is drawn as a break in the line and is never interpolated across.
ContinuityThe record begins in 1916 and is not continuous from it: 110 years separate the first value from the last, and 94% 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 Whitewater and what each holds
GaugeMeasuresValuesRecord
WHITEWATER RIVER AT BROOKVILLE, INcatchment area, annual maximum river flow, mean river flow, mean river flow, water year3151913–2026
WHITEWATER RIVER NEAR ALPINE, INcatchment area, annual maximum river flow, mean river flow, mean river flow, water year2911928–2026

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 — 05080003. 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
WHITEWATER RIVER AT BROOKVILLE, INStated 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
WHITEWATER RIVER NEAR ALPINE, INStated 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 2 of them, which makes it a profile, not indexed.

Information-gain signals held for this water body
SignalHeldCounts
Gauges holding a real record2no
Years spanned114yes, 20 or more
Values held606no
Distinct measurements4yes, 2 or more
Publishers measuring it1no
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), Whitewater gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-whitewater/

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 Whitewater 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 confidence2025-04-05

Source: USGS — National Water Information System, USGS site 03276500, 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.