The monitoring network within this area

Hydrionis holds 1,403 values from 6 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.

6
Gauges
1,403
Values held
1925–2026
Record spans
Gauges within the Lower Kootenai huc8 subbasin
6 monitoring points, positioned as the publisher records them.
Gauges within the Lower Kootenai huc8 subbasinKOOTENAI RIVER AT LEONIA, ID, BOUNDARY CREEK NR PORTHILL ID, KOOTENAI RIVER AT PORTHILL ID TOTAL FLOW, MYRTLE CREEK NR BONNERS FERRY ID, BALL CREEK NR BONNERS FERRY ID, KOOTENAI RIVER NR COPELAND IDKOOTENAI RIVER AT LEONIA, IDBOUNDARY CREEK NR PORTHILL IDKOOTENAI RIVER AT PORTHILL ID TOTAL FLOWMYRTLE CREEK NR BONNERS FERRY IDBALL CREEK NR BONNERS FERRY IDKOOTENAI RIVER NR COPELAND 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 BOUNDARY CREEK NR PORTHILL ID
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1929–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at BOUNDARY CREEK NR PORTHILL IDLargest measured flow of each year at BOUNDARY CREEK NR PORTHILL ID: BOUNDARY CREEK NR PORTHILL ID in m³/s, from 1929 to 2025.Hurricane Katrina water and sanitation collapse050100m³/s19291941195319651977199020032015

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
PeriodBOUNDARY CREEK NR PORTHILL ID (m³/s)
192936.8
193028.9
193137.4
193247.6
193368.0
193449.8
193545.3
193642.2
193737.4
193864.3
193939.6
194034.0
194165.1
194245.6
194368.0
194421.1
194552.1
194655.8
194748.1
194871.6
194960.0
195063.7
195145.9
195243.6
195364.3
195466.5
195592.9
195673.9
195751.3
195854.1
195953.8
196049.0
196189.8
196239.6
196347.0
196455.8
196550.4
196649.6
196763.1
1968100
196976.2
197052.4
197185.0
197279.6
197360.0
197492.3
197555.5
197684.1
197734.5
197852.7
197940.5
198092.6
198151.5
198266.3
198366.5
198558.3
198646.7
198775.6
198846.2
198960.9
199048.4
199171.6
199247.3
199353.5
199445.6
199549.8
1996106
1997107
199878.2
199980.7
200146.4
200276.2
200359.5
200444.5
200551.8
2006101
200763.1
200890.3
200955.8
201073.3
201158.9
201285.8
2013116
201459.7
201542.8
201645.9
201771.9
2018101
201935.4
202051.8
202141.9
202264.8
202396.3
20240
202545.3

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 held1929–2025
Completeness97.9% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 2 separate periods inside 1929–2025 hold no value. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1929 and is not continuous from it: 97 years separate the first value from the last, and 98% 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 KOOTENAI RIVER AT PORTHILL ID TOTAL FLOW, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1929–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above KOOTENAI RIVER AT PORTHILL ID TOTAL FLOW, as a depthWater leaving the catchment above KOOTENAI RIVER AT PORTHILL ID TOTAL FLOW, as a depth: KOOTENAI RIVER AT PORTHILL ID TOTAL FLOW in mm, from 1929 to 2025.Hurricane Katrina water and sanitation collapse200400600mm19291942195519681981199420072020

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
PeriodKOOTENAI RIVER AT PORTHILL ID TOTAL FLOW (mm)
1929276
1930310
1931232
1932426
1933514
1934493
1935387
1936291
1937296
1938419
1939318
1940280
1941283
1942413
1943437
1944203
1945296
1946446
1947482
1948500
1949346
1950515
1951558
1952404
1953407
1954559
1955429
1956540
1957368
1958348
1959545
1960425
1961484
1962374
1963385
1964422
1965437
1966416
1967476
1968404
1969509
1970299
1971483
1972531
1973238
1974583
1975402
1976458
1977274
1978359
1979288
1980345
1981460
1982443
1983404
1984346
1985333
1986401
1987307
1988330
1989353
1990484
1991552
1992283
1993313
1994283
1995449
1996567
1997533
1998368
1999484
2000357
2001196
2002432
2003321
2004340
2005369
2006441
2007433
2008365
2009295
2010314
2011490
2012567
2013419
2014454
2015323
2016401
2017461
2018400
2019262
2020392
2021321
2022410
2023274
2024309
2025292

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 held1929–2025
Completeness100.0% of the periods in that span are held.
ContinuityContinuous: every year from 1929 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.

1,208
Fullest snowpack recorded at Hidden Lake, in 2012 (mm of water)
471
Thinnest, in 2015 (mm of water)
April
Month the pack is usually at its fullest
June
Month the pack has gone by, in half of years
Peak snowpack at Hidden Lake
Water years 2001–2026. Each point is the fullest month of that snow season.
Peak snowpack at Hidden LakePeak snowpack at Hidden Lake: Hidden Lake in mm, from 2001 to 2026.05001,000mm2001200520092013201720212025Hidden Lake 2001: 484 mmHidden Lake 2002: 991 mmHidden Lake 2003: 818 mmHidden Lake 2004: 836 mmHidden Lake 2005: 488 mmHidden Lake 2006: 1,090 mmHidden Lake 2007: 871 mmHidden Lake 2008: 945 mmHidden Lake 2009: 750 mmHidden Lake 2010: 847 mmHidden Lake 2011: 1,165 mmHidden Lake 2012: 1,208 mmHidden Lake 2013: 825 mmHidden Lake 2014: 1,003 mmHidden Lake 2015: 471 mmHidden Lake 2016: 827 mmHidden Lake 2017: 848 mmHidden Lake 2018: 1,166 mmHidden Lake 2019: 672 mmHidden Lake 2020: 1,001 mmHidden Lake 2021: 770 mmHidden Lake 2022: 833 mmHidden Lake 2023: 737 mmHidden Lake 2024: 748 mmHidden Lake 2025: 825 mmHidden Lake 2026: 634 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
PeriodHidden Lake (mm)
2001484
2002991
2003818
2004836
2005488
20061,090
2007871
2008945
2009750
2010847
20111,165
20121,208
2013825
20141,003
2015471
2016827
2017848
20181,166
2019672
20201,001
2021770
2022833
2023737
2024748
2025825
2026634

Read against the river

Hidden Lake and KOOTENAI RIVER AT LEONIA, ID both sit in this drainage area, and their records overlap by 24 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 Lower Kootenai and what each holds
GaugeMeasuresValuesRecord
BOUNDARY CREEK NR PORTHILL IDburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3241929–2026
KOOTENAI RIVER AT LEONIA, IDburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2381928–2026
KOOTENAI RIVER AT PORTHILL ID TOTAL FLOWburned area within 50 km, catchment area, mean river flow, mean river flow, water year2311928–2026
KOOTENAI RIVER NR COPELAND IDcatchment area, annual maximum river flow111925–2026
BALL CREEK NR BONNERS FERRY IDcatchment area, annual maximum river flow91972–2026
MYRTLE CREEK NR BONNERS FERRY IDcatchment area, annual maximum river flow22002–2026

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 — 17010104. 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
BOUNDARY CREEK NR PORTHILL 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
KOOTENAI RIVER AT LEONIA, 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
KOOTENAI RIVER AT PORTHILL ID TOTAL FLOWStated 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
KOOTENAI RIVER NR COPELAND 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
BALL CREEK NR BONNERS FERRY 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
MYRTLE CREEK NR BONNERS FERRY 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 5 of them, which makes it a full profile.

Information-gain signals held for this water body
SignalHeldCounts
Gauges holding a real record3yes, 3 or more
Years spanned102yes, 20 or more
Values held1,403yes, 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), Lower Kootenai gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-lower-kootenai/

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 Kootenai 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 confidence2025-05-29

Source: USGS — National Water Information System, USGS site 12321500, 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.