The monitoring network within this area

Hydrionis holds 342 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
342
Values held
1913–2026
Record spans
Gauges within the Lower Coosa huc8 subbasin
2 monitoring points, positioned as the publisher records them.
Gauges within the Lower Coosa huc8 subbasinCOOSA RIVER AT CHILDERSBURG AL, COOSA RIVER AT JORDAN DAM NEAR WETUMPKA ALCOOSA RIVER AT CHILDERSBURG ALCOOSA RIVER AT JORDAN DAM NEAR WETUMPKA AL

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 COOSA RIVER AT CHILDERSBURG AL
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1916–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at COOSA RIVER AT CHILDERSBURG ALLargest measured flow of each year at COOSA RIVER AT CHILDERSBURG AL: COOSA RIVER AT CHILDERSBURG AL in m³/s, from 1916 to 2025.Hurricane Katrina water and sanitation collapse02,0004,000m³/s19161929194519601982199620082021

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 recordA 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 collapseFlood2005-08-292005-09-30Documented record
Compiled record

Not shown on this chart

  • The 1976 droughtThis 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 droughtThis event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • Yorkshire droughtThis 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 PauloThis 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 ZeroThis event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • European droughtThis 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
PeriodCOOSA RIVER AT CHILDERSBURG AL (m³/s)
19163,426
19172,710
19181,945
19193,285
19212,619
19222,730
19232,461
19241,518
19252,520
19261,552
19272,027
19282,350
19293,228
19301,447
19322,030
19342,616
19363,681
19372,667
19383,851
19391,911
19401,365
1941926
19422,410
19442,625
19451,407
19463,200
19473,596
19482,353
19502,220
19514,134
19532,410
19542,044
19552,061
19562,135
19572,574
19591,257
19601,461
19613,964
19632,509
19642,396
19651,699
19662,152
19671,620
19691,583
19762,220
19794,248
19802,818
19811,481
19821,773
19832,294
19851,671
1986898
19871,804
19881,368
19892,396
19903,115
19911,804
19921,608
19941,838
19951,869
19962,549
19970
19980
19990
20000
20010
20020
20030
20040
20050
20060
20070
20080
20090
20100
20110
20121,192
20132,209
20142,254
20151,841
20171,090
20181,829
20192,772
20202,820
20212,353
20222,379
20232,093
20242,002
20252,112

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 held19162025
Completeness80.9% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 15 separate periods inside 1916–2025 hold no value. The longest runs from 1970 to 1975 — 6 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1916 and is not continuous from it: 110 years separate the first value from the last, and 81% of the years between them are held. The span is not the record.
Last read from the publisher2026-08-31
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 COOSA RIVER AT JORDAN DAM NEAR WETUMPKA AL, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1913–2012.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above COOSA RIVER AT JORDAN DAM NEAR WETUMPKA AL, as a depthWater leaving the catchment above COOSA RIVER AT JORDAN DAM NEAR WETUMPKA AL, as a depth: COOSA RIVER AT JORDAN DAM NEAR WETUMPKA AL in mm, from 1913 to 2012.Hurricane Katrina water and sanitation collapse02505007501,000mm19131937194819591970198119922003

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 recordA 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 collapseFlood2005-08-292005-09-30Documented record
Compiled record

Not shown on this chart

  • The 1976 droughtThis 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 droughtThis event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • Yorkshire droughtThis 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 PauloThis 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 ZeroThis event’s area does not contain this chart’s subject. Sharing a country is not sharing an event, so it is not drawn.
  • European droughtThis 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
PeriodCOOSA RIVER AT JORDAN DAM NEAR WETUMPKA AL (mm)
1913493
1927416
1928531
1929882
1930413
1931329
1932828
1933544
1934453
1935466
1936746
1937653
1938541
1939513
1940439
1941330
1942505
1943524
1944590
1945508
1946836
1947590
1948749
1949696
1950507
1951620
1952521
1953562
1954372
1955425
1956452
1957627
1958464
1959435
1960443
1961747
1962615
1963584
1964796
1965441
1966564
1967611
1968508
1969461
1970418
1971601
1972595
1973766
1974590
1975809
1976677
1977686
1978440
1979871
1980735
1981323
1982728
1983764
1984607
1985342
1986218
1987388
1988261
1989739
1990733
1991506
1992583
1993475
1994596
1995565
1996646
1997647
1998615
1999391
2000291
2001463
2002480
2003738
2004533
2005503
2006337
2007157
2008278
2009773
2010468
2011410
2012300

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 held19132012
Completeness87.0% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • One period inside 1913–2012 holds no value: 1914 to 1926, 13 years with no reading. It is drawn as a break in the line and is never interpolated across.
ContinuityThe record begins in 1913 and is not continuous from it: 100 years separate the first value from the last, and 87% of the years between them are held. The span is not the record.
Last read from the publisher2026-08-24
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 Lower Coosa and what each holds
GaugeMeasuresValuesRecord
COOSA RIVER AT CHILDERSBURG ALburned area within 50 km, catchment area, annual maximum river flow, mean river flow2091914–2026
COOSA RIVER AT JORDAN DAM NEAR WETUMPKA ALcatchment area, annual maximum river flow, mean river flow1331913–2026

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 — 03150107. 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
COOSA RIVER AT CHILDERSBURG ALStated 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/42026-08-26
COOSA RIVER AT JORDAN DAM NEAR WETUMPKA ALStated 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/42026-08-26

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 3 of them, which makes it a full profile.

Information-gain signals held for this water body
SignalHeldCounts
Gauges holding a real record2no
Years spanned114yes, 20 or more
Values held342no
Distinct measurements4yes, 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 Coosa gauge records, accessed 2026-09-02, hydrionis.com/waters/united-states-lower-coosa/

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 Coosa 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 confidence2025-02-13

Source: USGSNational Water Information System, USGS site 02407000, 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 31 August 2026.