The monitoring network within this area

Hydrionis holds 302 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
302
Values held
1903–2026
Record spans
Gauges within the Toledo Bend Reservoir huc8 subbasin
2 monitoring points, positioned as the publisher records them.
Gauges within the Toledo Bend Reservoir huc8 subbasinSabine Rv at Logansport, LA, Bayou San Patricio near Benson, LASabine Rv at Logansport, LABayou San Patricio near Benson, LA

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 Sabine Rv at Logansport, LA
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1904–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at Sabine Rv at Logansport, LALargest measured flow of each year at Sabine Rv at Logansport, LA: Sabine Rv at Logansport, LA in m³/s, from 1904 to 2025.Hurricane Katrina water and sanitation collapse01,0002,0003,000m³/s19041916192819421955196820072020

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
PeriodSabine Rv at Logansport, LA (m³/s)
1904172
1905951
1906566
1907306
1908852
1909179
1910214
1911198
1912459
1913337
19141,019
19151,331
1916391
1917144
1918252
1919303
1920895
19211,178
1922929
1923345
1924396
192587.8
1926651
1927592
1928279
1929340
1930985
1931306
19321,164
1933833
1934493
19351,019
1937334
1938728
1939385
1940228
1942765
1943889
1944971
19452,605
19461,048
1948374
1949266
1950818
1951216
1952368
19531,158
1954326
1955357
1956391
19571,736
19581,453
1959430
1960402
1961396
1963199
1964164
1965320
19661,325
1967235
1968297
19930
19940
19950
19980
19990
20000
20010
20020
20030
20040
20060
20070
20080
20090
20110
20120
20130
20140
20150
20160
20170
20180
2019991
2020541
2021886
2022408
2023586
20241,416
2025561

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 held1904–2025
Completeness73.8% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 8 separate periods inside 1904–2025 hold no value. The longest runs from 1969 to 1992 — 24 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1904 and is not continuous from it: 122 years separate the first value from the last, and 74% 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 Sabine Rv at Logansport, LA, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1904–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above Sabine Rv at Logansport, LA, as a depthWater leaving the catchment above Sabine Rv at Logansport, LA, as a depth: Sabine Rv at Logansport, LA in mm, from 1904 to 2025.Hurricane Katrina water and sanitation collapse0200400600800mm19041913192219311940194919581967Sabine Rv at Logansport, LA 1904: 87.0 mmSabine Rv at Logansport, LA 1905: 500 mmSabine Rv at Logansport, LA 1906: 281 mmSabine Rv at Logansport, LA 1907: 241 mmSabine Rv at Logansport, LA 1908: 255 mmSabine Rv at Logansport, LA 1909: 54.0 mmSabine Rv at Logansport, LA 1910: 70.0 mmSabine Rv at Logansport, LA 1911: 57.0 mmSabine Rv at Logansport, LA 1912: 173 mmSabine Rv at Logansport, LA 1913: 209 mmSabine Rv at Logansport, LA 1914: 275 mmSabine Rv at Logansport, LA 1915: 363 mmSabine Rv at Logansport, LA 1916: 159 mmSabine Rv at Logansport, LA 1917: 70.0 mmSabine Rv at Logansport, LA 1918: 85.0 mmSabine Rv at Logansport, LA 1919: 408 mmSabine Rv at Logansport, LA 1920: 264 mmSabine Rv at Logansport, LA 1921: 251 mmSabine Rv at Logansport, LA 1922: 291 mmSabine Rv at Logansport, LA 1923: 204 mmSabine Rv at Logansport, LA 1924: 216 mmSabine Rv at Logansport, LA 1925: 65.0 mmSabine Rv at Logansport, LA 1926: 244 mmSabine Rv at Logansport, LA 1927: 260 mmSabine Rv at Logansport, LA 1928: 151 mmSabine Rv at Logansport, LA 1929: 228 mmSabine Rv at Logansport, LA 1930: 234 mmSabine Rv at Logansport, LA 1931: 154 mmSabine Rv at Logansport, LA 1932: 345 mmSabine Rv at Logansport, LA 1933: 253 mmSabine Rv at Logansport, LA 1934: 189 mmSabine Rv at Logansport, LA 1935: 281 mmSabine Rv at Logansport, LA 1936: 62.0 mmSabine Rv at Logansport, LA 1937: 176 mmSabine Rv at Logansport, LA 1938: 289 mmSabine Rv at Logansport, LA 1939: 136 mmSabine Rv at Logansport, LA 1940: 257 mmSabine Rv at Logansport, LA 1941: 408 mmSabine Rv at Logansport, LA 1942: 323 mmSabine Rv at Logansport, LA 1943: 168 mmSabine Rv at Logansport, LA 1944: 424 mmSabine Rv at Logansport, LA 1945: 623 mmSabine Rv at Logansport, LA 1946: 557 mmSabine Rv at Logansport, LA 1947: 257 mmSabine Rv at Logansport, LA 1948: 243 mmSabine Rv at Logansport, LA 1949: 237 mmSabine Rv at Logansport, LA 1950: 368 mmSabine Rv at Logansport, LA 1951: 99.0 mmSabine Rv at Logansport, LA 1952: 186 mmSabine Rv at Logansport, LA 1953: 286 mmSabine Rv at Logansport, LA 1954: 107 mmSabine Rv at Logansport, LA 1955: 144 mmSabine Rv at Logansport, LA 1956: 73.0 mmSabine Rv at Logansport, LA 1957: 468 mmSabine Rv at Logansport, LA 1958: 316 mmSabine Rv at Logansport, LA 1959: 190 mmSabine Rv at Logansport, LA 1960: 278 mmSabine Rv at Logansport, LA 1961: 312 mmSabine Rv at Logansport, LA 1962: 172 mmSabine Rv at Logansport, LA 1963: 60.0 mmSabine Rv at Logansport, LA 1964: 39.0 mmSabine Rv at Logansport, LA 1965: 146 mmSabine Rv at Logansport, LA 1966: 246 mmSabine Rv at Logansport, LA 1967: 90.0 mmSabine Rv at Logansport, LA 2019: 450 mmSabine Rv at Logansport, LA 2020: 268 mmSabine Rv at Logansport, LA 2021: 317 mmSabine Rv at Logansport, LA 2022: 95.0 mmSabine Rv at Logansport, LA 2023: 192 mmSabine Rv at Logansport, LA 2024: 457 mmSabine Rv at Logansport, LA 2025: 296 mm

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
PeriodSabine Rv at Logansport, LA (mm)
190487.0
1905500
1906281
1907241
1908255
190954.0
191070.0
191157.0
1912173
1913209
1914275
1915363
1916159
191770.0
191885.0
1919408
1920264
1921251
1922291
1923204
1924216
192565.0
1926244
1927260
1928151
1929228
1930234
1931154
1932345
1933253
1934189
1935281
193662.0
1937176
1938289
1939136
1940257
1941408
1942323
1943168
1944424
1945623
1946557
1947257
1948243
1949237
1950368
195199.0
1952186
1953286
1954107
1955144
195673.0
1957468
1958316
1959190
1960278
1961312
1962172
196360.0
196439.0
1965146
1966246
196790.0
2019450
2020268
2021317
202295.0
2023192
2024457
2025296

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 held1904–2025
Completeness58.2% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • One period inside 1904–2025 holds no value: 1968 to 2018, 51 years with no reading. It is drawn as a break in the line and is never interpolated across.
ContinuityThe record begins in 1904 and is not continuous from it: 122 years separate the first value from the last, and 58% 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 Toledo Bend Reservoir and what each holds
GaugeMeasuresValuesRecord
Sabine Rv at Logansport, LAcatchment area, annual maximum river flow, mean river flow, mean river flow, water year2391903–2026
Bayou San Patricio near Benson, LAcatchment area, annual maximum river flow631954–2026

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 — 12010004. 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
Sabine Rv at Logansport, LAStated 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
Bayou San Patricio near Benson, LAStated 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 spanned124yes, 20 or more
Values held302no
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), Toledo Bend Reservoir gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-toledo-bend-reservoir/

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 Toledo Bend Reservoir 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 confidence2025-05-07

Source: USGS — National Water Information System, USGS site 08022500, 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.