The monitoring network within this area

Hydrionis holds 1,149 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
1,149
Values held
1889–2026
Record spans
Gauges within the Conococheague-Opequon huc8 subbasin
4 monitoring points, positioned as the publisher records them.
Gauges within the Conococheague-Opequon huc8 subbasinCONOCOCHEAGUE CREEK AT FAIRVIEW, MD, ANTIETAM CREEK NEAR SHARPSBURG, MD, BACK CREEK NEAR JONES SPRINGS, WV, POTOMAC RIVER AT SHEPHERDSTOWN, WVCONOCOCHEAGUE CREEK AT FAIRVIEW, MDANTIETAM CREEK NEAR SHARPSBURG, MDBACK CREEK NEAR JONES SPRINGS, WVPOTOMAC RIVER AT SHEPHERDSTOWN, WV

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 CONOCOCHEAGUE CREEK AT FAIRVIEW, 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 CONOCOCHEAGUE CREEK AT FAIRVIEW, MDLargest measured flow of each year at CONOCOCHEAGUE CREEK AT FAIRVIEW, MD: CONOCOCHEAGUE CREEK AT FAIRVIEW, MD in m³/s, from 1889 to 2025.Hurricane Katrina water and sanitation collapse02505007501,000m³/s18891941195519671981199320062018

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
PeriodCONOCOCHEAGUE CREEK AT FAIRVIEW, MD (m³/s)
1889623
1924368
1929220
1931127
1932133
1933255
1934303
1936388
1937402
1939185
1940193
1941118
1942182
1944160
1945225
1946178
1947133
1948124
1949189
1950150
1952439
1954130
1955221
1956123
1958213
1959146
1960183
1961273
1962146
1963252
1964177
1965314
1966340
1967237
1968117
1969133
1970306
1971212
1972917
1973165
1975447
1976510
1978208
1979354
1981184
1982129
1983166
1984609
1985166
1986277
1987220
1988236
1989219
1990143
1992121
1993311
1995131
1996473
1997385
1999177
2000155
2001114
200258.6
2003411
2004394
2005276
2006210
2007199
2008276
2009145
2010408
2011382
2012274
2014442
2015135
2016174
2017151
2018286
2019177
2020144
2022204
2024247
2025276

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
Completeness60.6% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 18 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 61% 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 CONOCOCHEAGUE CREEK AT FAIRVIEW, 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. 1929–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above CONOCOCHEAGUE CREEK AT FAIRVIEW, MD, as a depthWater leaving the catchment above CONOCOCHEAGUE CREEK AT FAIRVIEW, MD, as a depth: CONOCOCHEAGUE CREEK AT FAIRVIEW, MD in mm, from 1929 to 2025.Hurricane Katrina water and sanitation collapse02505007501,000mm19291942195519681981199420072020

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
PeriodCONOCOCHEAGUE CREEK AT FAIRVIEW, MD (mm)
1929479
1930186
1931229
1932364
1933484
1934400
1935327
1936518
1937609
1938221
1939351
1940440
1941268
1942597
1943403
1944343
1945434
1946385
1947331
1948379
1949365
1950552
1951492
1952665
1953468
1954270
1955369
1956416
1957307
1958445
1959240
1960372
1961412
1962317
1963266
1964321
1965270
1966232
1967415
1968331
1969204
1970620
1971496
1972801
1973717
1974439
1975705
1976472
1977357
1978492
1979692
1980345
1981291
1982352
1983488
1984597
1985335
1986339
1987298
1988297
1989424
1990358
1991299
1992358
1993666
1994621
1995328
1996971
1997384
1998635
1999316
2000324
2001239
2002235
2003819
2004632
2005407
2006366
2007302
2008477
2009375
2010450
2011716
2012436
2013349
2014454
2015268
2016296
2017381
2018902
2019567
2020330
2021353
2022334
2023231
2024453
2025323

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

Every gauge Hydrionis holds within this area

Gauges within the Conococheague-Opequon and what each holds
GaugeMeasuresValuesRecord
CONOCOCHEAGUE CREEK AT FAIRVIEW, MDburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3301889–2026
ANTIETAM CREEK NEAR SHARPSBURG, MDburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3251928–2026
POTOMAC RIVER AT SHEPHERDSTOWN, WVburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2711889–2026
BACK CREEK NEAR JONES SPRINGS, WVburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year2231928–2026

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 — 02070004. 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
CONOCOCHEAGUE CREEK AT FAIRVIEW, 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
ANTIETAM CREEK NEAR SHARPSBURG, 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
POTOMAC RIVER AT SHEPHERDSTOWN, WVStated 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
BACK CREEK NEAR JONES SPRINGS, WVStated 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 record4yes, 3 or more
Years spanned138yes, 20 or more
Values held1,149yes, 1000 or more
Distinct measurements5yes, 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), Conococheague-Opequon gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-conococheague-opequon/

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 Conococheague-Opequon 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 01614500, 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.