The monitoring network within this area

Hydrionis holds 537 values from 3 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.

3
Gauges
537
Values held
1917–2026
Record spans
Gauges within the Molokai huc8 subbasin
3 monitoring points, positioned as the publisher records them.
Gauges within the Molokai huc8 subbasinHalawa Stream near Halawa, Molokai, HI, Waikolu Str blw pipe nr Kalaupapa, Molokai, HI, PELEKUNU STREAM NR PELEKUNU, MOLOKAI, HIHalawa Stream near Halawa, Molokai, HIWaikolu Str blw pipe nr Kalaupapa, Molokai, HIPELEKUNU STREAM NR PELEKUNU, MOLOKAI, HI

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 Halawa Stream near Halawa, Molokai, HI
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1918–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at Halawa Stream near Halawa, Molokai, HILargest measured flow of each year at Halawa Stream near Halawa, Molokai, HI: Halawa Stream near Halawa, Molokai, HI in m³/s, from 1918 to 2025.Hurricane Katrina water and sanitation collapse0200400600800m³/s19181939195219651978199020042015

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
PeriodHalawa Stream near Halawa, Molokai, HI (m³/s)
191832.0
192047.0
192139.9
192368.0
192422.8
1927171
192925.4
193082.4
1938140
1939104
194069.1
1941137
1943223
194443.9
1946123
1948277
194994.3
195091.2
1952109
195487.5
1955175
1957105
195974.5
196074.5
1961309
1963108
196442.5
1965762
196687.8
196872.8
196981.3
197069.9
197250.1
197327.9
197450.4
197653.5
1978141
197968.8
198150.4
198269.1
198345.9
198580.1
198674.2
198757.5
198967.1
199060.0
199166.8
199262.3
199455.2
199541.6
199638.8
199817.5
200088.3
200266.8
200474.8
200682.7
200768.2
200868.8
200969.4
201066.8
201165.4
201363.7
201489.2
201574.2
201653.5
201762.0
201876.2
202063.1
202175.6
202351.5
202478.4
202584.7

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 held1918–2025
Completeness66.7% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 29 separate periods inside 1918–2025 hold no value. The longest runs from 1931 to 1937 — 7 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1918 and is not continuous from it: 108 years separate the first value from the last, and 67% 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 Halawa Stream near Halawa, Molokai, HI, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1918–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above Halawa Stream near Halawa, Molokai, HI, as a depthWater leaving the catchment above Halawa Stream near Halawa, Molokai, HI, as a depth: Halawa Stream near Halawa, Molokai, HI in mm, from 1918 to 2025.Hurricane Katrina water and sanitation collapse1,0002,0003,000mm19181939195219651978199120042017

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
PeriodHalawa Stream near Halawa, Molokai, HI (mm)
19182,932
19212,674
19222,166
19232,483
19241,640
19251,864
19261,459
19272,711
19282,157
19292,026
19302,498
19311,967
19382,932
19392,822
19402,290
19412,741
19422,888
19432,490
19441,906
19451,503
19462,276
19472,306
19482,889
19491,658
19502,232
19511,893
19522,187
19531,481
19542,107
19552,424
19562,179
19572,129
19582,321
19591,864
19602,298
19613,293
19622,416
19633,094
19643,088
19652,608
19661,849
19671,938
19682,046
19692,291
19701,982
19711,319
19721,507
19731,753
19741,606
19751,201
19761,795
19771,540
19782,262
19792,269
19802,756
19811,923
19823,337
19831,739
19841,167
19851,871
19862,439
19872,932
19882,645
19892,969
19902,881
19912,026
19922,475
19931,974
19942,416
19951,650
19961,899
19972,453
19981,857
19991,599
20001,839
20011,790
20022,085
20031,820
20042,563
20052,070
20062,313
20071,739
20081,337
20091,753
20101,650
20111,473
20121,411
20131,901
20142,976
20152,748
20163,376
20171,989
20183,190
20191,761
20202,142
20212,380
20221,378
20231,886
20241,588
20251,326

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 held1918–2025
Completeness92.6% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 2 separate periods inside 1918–2025 hold no value. The longest runs from 1932 to 1937 — 6 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1918 and is not continuous from it: 108 years separate the first value from the last, and 93% 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 Molokai and what each holds
GaugeMeasuresValuesRecord
Halawa Stream near Halawa, Molokai, HIcatchment area, annual maximum river flow, mean river flow, mean river flow, water year3011917–2026
Waikolu Str blw pipe nr Kalaupapa, Molokai, HIcatchment area, annual maximum river flow, mean river flow, mean river flow, water year2071920–2026
PELEKUNU STREAM NR PELEKUNU, MOLOKAI, HIcatchment area, annual maximum river flow291920–2026

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 — 20050000. 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
Halawa Stream near Halawa, Molokai, HIStated 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
Waikolu Str blw pipe nr Kalaupapa, Molokai, HIStated 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
PELEKUNU STREAM NR PELEKUNU, MOLOKAI, HIStated 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 spanned110yes, 20 or more
Values held537no
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), Molokai gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-molokai/

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 Molokai 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 confidence2025-04-18

Source: USGS — National Water Information System, USGS site 16400000, 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.