The monitoring network within this area

Hydrionis holds 848 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
848
Values held
1835–2026
Record spans
Gauges within the Lower Genesee huc8 subbasin
4 monitoring points, positioned as the publisher records them.
Gauges within the Lower Genesee huc8 subbasinGENESEE RIVER NEAR MOUNT MORRIS NY, GENESEE RIVER AT FORD STREET BRIDGE, ROCHESTER NY, GENESEE RIVER AT ROCHESTER NY, CONESUS CREEK NEAR LAKEVILLE NYGENESEE RIVER NEAR MOUNT MORRIS NYGENESEE RIVER AT FORD STREET BRIDGE, ROCHESTER NYGENESEE RIVER AT ROCHESTER NYCONESUS CREEK NEAR LAKEVILLE NY

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 GENESEE RIVER NEAR MOUNT MORRIS NY
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1890–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at GENESEE RIVER NEAR MOUNT MORRIS NYLargest measured flow of each year at GENESEE RIVER NEAR MOUNT MORRIS NY: GENESEE RIVER NEAR MOUNT MORRIS NY in m³/s, from 1890 to 2025.Hurricane Katrina water and sanitation collapse05001,0001,5002,000m³/s18901920193519501966198119972011

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
PeriodGENESEE RIVER NEAR MOUNT MORRIS NY (m³/s)
1890566
18941,189
1904340
1905425
1909680
1910510
1911396
1912467
19131,076
1914532
19161,560
1917900
1918821
1919906
1920586
1921507
1922413
1923345
1924569
1925753
1926411
1927470
1929736
1930555
1931368
1932453
1933513
1934405
1935411
1936745
1937510
1938510
1939722
1940838
1941697
1942917
1944481
1945631
1946654
1947866
1948784
1949362
19501,286
1952269
1954391
1955362
1956337
1957328
1958303
1959343
1960294
1961261
1962278
1963297
1964311
1965242
1966237
1967207
1968244
1969252
1970212
1971237
1972504
1974228
1975224
1976283
1977294
1978292
1979269
1980244
1981269
1982292
1983262
1984297
1985241
1987256
1988167
1989277
1990183
1992204
1993267
1994275
1995167
1996222
1997217
1998241
1999208
2000178
2001205
2002177
2003215
2004202
2005192
2006201
2007216
2008195
2009242
2010224
2011238
2012195
2014216
2015209
2016168
2017206
2018205
2020198
2021168
2023179
2024196
2025196

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 held1890–2025
Completeness80.9% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 14 separate periods inside 1890–2025 hold no value. The longest runs from 1895 to 1903 — 9 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1890 and is not continuous from it: 136 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 publisher2026-10-01
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 GENESEE RIVER AT ROCHESTER NY, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1906–2004.
Water leaving the catchment above GENESEE RIVER AT ROCHESTER NY, as a depthWater leaving the catchment above GENESEE RIVER AT ROCHESTER NY, as a depth: GENESEE RIVER AT ROCHESTER NY in mm, from 1906 to 2004.200400600mm19061925193719491961197319851997

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 (0 events)

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
PeriodGENESEE RIVER AT ROCHESTER NY (mm)
1906324
1911362
1912318
1913377
1915314
1916502
1917383
1920299
1921311
1922307
1923310
1924401
1925367
1926377
1927547
1928424
1929470
1930378
1931310
1932400
1933342
1934233
1935339
1936388
1937407
1938338
1939344
1940402
1941273
1942452
1943502
1944334
1945615
1946361
1947521
1948370
1949272
1950445
1951435
1952397
1953316
1954346
1955362
1956540
1957333
1958329
1959448
1960401
1961350
1962266
1963262
1964299
1965260
1966315
1967411
1968346
1969394
1970426
1971358
1972661
1973422
1974429
1975470
1976555
1977598
1978420
1979523
1980355
1981459
1982477
1983385
1984561
1985374
1986394
1987341
1988229
1989375
1990485
1991326
1992465
1993422
1994406
1995247
1996564
1997380
1998409
1999248
2000382
2001260
2002368
2003522
2004545

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 held1906–2004
Completeness92.9% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 3 separate periods inside 1906–2004 hold no value. The longest runs from 1907 to 1910 — 4 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1906 and is not continuous from it: 99 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 Lower Genesee and what each holds
GaugeMeasuresValuesRecord
GENESEE RIVER AT ROCHESTER NYcatchment area, annual maximum river flow, mean river flow, mean river flow, water year2861835–2026
GENESEE RIVER NEAR MOUNT MORRIS NYcatchment area, annual maximum river flow, mean river flow, mean river flow, water year2681890–2026
GENESEE RIVER AT FORD STREET BRIDGE, ROCHESTER NYcatchment area, annual maximum river flow, mean river flow, mean river flow, water year2491835–2026
CONESUS CREEK NEAR LAKEVILLE NYcatchment area, annual maximum river flow451920–2026

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 — 04130003. 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
GENESEE RIVER AT ROCHESTER NYStated 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
GENESEE RIVER NEAR MOUNT MORRIS NYStated 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
GENESEE RIVER AT FORD STREET BRIDGE, ROCHESTER NYStated 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
CONESUS CREEK NEAR LAKEVILLE NYStated 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 3 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 spanned192yes, 20 or more
Values held848no
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), Lower Genesee gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-lower-genesee/

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 Genesee 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 confidence2005-04-04

Source: USGS — National Water Information System, USGS site 04232000, 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.