The monitoring network within this area

Hydrionis holds 1,120 values from 4 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.

4
Gauges
1,120
Values held
1889–2026
Record spans
Gauges within the North Branch Potomac huc8 subbasin
4 monitoring points, positioned as the publisher records them.
Gauges within the North Branch Potomac huc8 subbasinNORTH BRANCH POTOMAC RIVER AT LUKE, MD, GEORGES CREEK AT FRANKLIN, MD, WILLS CREEK NEAR CUMBERLAND, MD, NORTH BRANCH POTOMAC RIVER NEAR CUMBERLAND, MDNORTH BRANCH POTOMAC RIVER AT LUKE, MDGEORGES CREEK AT FRANKLIN, MDWILLS CREEK NEAR CUMBERLAND, MDNORTH BRANCH POTOMAC RIVER NEAR CUMBERLAND, MD

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 NORTH BRANCH POTOMAC RIVER NEAR CUMBERLAND, MD
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1889–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at NORTH BRANCH POTOMAC RIVER NEAR CUMBERLAND, MDLargest measured flow of each year at NORTH BRANCH POTOMAC RIVER NEAR CUMBERLAND, MD: NORTH BRANCH POTOMAC RIVER NEAR CUMBERLAND, MD in m³/s, from 1889 to 2025.Hurricane Katrina water and sanitation collapse01,0002,0003,000m³/s18891940195319651978199020032016

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
PeriodNORTH BRANCH POTOMAC RIVER NEAR CUMBERLAND, MD (m³/s)
18892,520
19242,322
1929311
1931382
1932799
1933663
1934476
1935362
19362,498
19371,464
1939609
1940476
1941589
1942476
1944433
1945515
1946244
1947268
1948555
1950337
1951654
1952586
1953326
1954538
1956467
1957530
1958487
1959216
1960629
1961716
1962575
1963665
1964753
1965270
1966416
1967719
1968566
1969206
1970629
1971385
1972493
1974394
1975535
1976320
1978665
1979578
1980388
1981394
1982371
1983428
1984654
1985249
1987272
1988425
1989385
1990272
1992182
1993733
1994422
1995402
19961,676
1998419
1999252
2000343
2001309
2002219
2003462
2004555
2005682
2007257
2008362
2009665
2010665
2011617
2012269
2014430
2015377
2016236
2017343
2018711
2020379
2021702
2022470
2023156
2024572
20251,113

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 held1889–2025
Completeness62.8% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 15 separate periods inside 1889–2025 hold no value. The longest runs from 1890 to 1923 — 34 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1889 and is not continuous from it: 137 years separate the first value from the last, and 63% 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 GEORGES CREEK AT FRANKLIN, MD, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1930–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above GEORGES CREEK AT FRANKLIN, MD, as a depthWater leaving the catchment above GEORGES CREEK AT FRANKLIN, MD, as a depth: GEORGES CREEK AT FRANKLIN, MD in mm, from 1930 to 2025.Hurricane Katrina water and sanitation collapse02505007501,000mm19301942195419661978199020022014

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
PeriodGEORGES CREEK AT FRANKLIN, MD (mm)
1930126
1931250
1932318
1933415
1934234
1935393
1936542
1937609
1938220
1939303
1940394
1941280
1942477
1943283
1944356
1945440
1946327
1947240
1948480
1949390
1950399
1951453
1952474
1953375
1954271
1955420
1956480
1957376
1958383
1959294
1960417
1961498
1962391
1963334
1964387
1965343
1966257
1967381
1968335
1969155
1970481
1971495
1972675
1973507
1974413
1975589
1976338
1977346
1978521
1979623
1980389
1981337
1982378
1983442
1984565
1985455
1986325
1987305
1988320
1989514
1990392
1991293
1992254
1993506
1994571
1995327
1996785
1997353
1998555
1999237
2000278
2001335
2002261
2003835
2004579
2005369
2006318
2007352
2008512
2009422
2010413
2011708
2012324
2013396
2014299
2015332
2016310
2017460
20181,014
2019520
2020405
2021300
2022343
2023236
2024427
2025482

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 held1930–2025
Completeness100.0% of the periods in that span are held.
ContinuityContinuous: every year from 1930 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

Every gauge Hydrionis holds within this area

Gauges within the North Branch Potomac and what each holds
GaugeMeasuresValuesRecord
NORTH BRANCH POTOMAC RIVER NEAR CUMBERLAND, MDcatchment area, annual maximum river flow, mean river flow, mean river flow, water year2911889–2026
WILLS CREEK NEAR CUMBERLAND, MDcatchment area, annual maximum river flow, mean river flow, mean river flow, water year2901924–2026
GEORGES CREEK AT FRANKLIN, MDcatchment area, annual maximum river flow, mean river flow, mean river flow, water year2891924–2026
NORTH BRANCH POTOMAC RIVER AT LUKE, MDcatchment area, annual maximum river flow, mean river flow, mean river flow, water year2501899–2026

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 — 02070002. 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
NORTH BRANCH POTOMAC RIVER NEAR CUMBERLAND, MDStated 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
WILLS CREEK NEAR CUMBERLAND, MDStated 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
GEORGES CREEK AT FRANKLIN, MDStated 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
NORTH BRANCH POTOMAC RIVER AT LUKE, MDStated 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 4 of them, which makes it a full profile.

Information-gain signals held for this water body
SignalHeldCounts
Gauges holding a real record4yes, 3 or more
Years spanned138yes, 20 or more
Values held1,120yes, 1000 or more
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), North Branch Potomac gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-north-branch-potomac/

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 North Branch Potomac 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 confidence2025-05-14

Source: USGS — National Water Information System, USGS site 01603000, 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.