The monitoring network within this area

Hydrionis holds 2,767 values from 8 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.

8
Gauges
2,767
Values held
1810–2026
Record spans
Gauges within the Upper French Broad huc8 subbasin
8 monitoring points, positioned as the publisher records them.
Gauges within the Upper French Broad huc8 subbasinFRENCH BROAD RIVER AT ROSMAN, NC, DAVIDSON RIVER NEAR BREVARD, NC, FRENCH BROAD RIVER AT BLANTYRE, NC, MILLS RIVER NEAR MILLS RIVER, NC, BEETREE CREEK NEAR SWANNANOA, NC, SWANNANOA RIVER AT BILTMORE, NC, FRENCH BROAD RIVER AT ASHEVILLE, NC, FRENCH BROAD RIVER NEAR NEWPORT, TNFRENCH BROAD RIVER AT ROSMAN, NCDAVIDSON RIVER NEAR BREVARD, NCFRENCH BROAD RIVER AT BLANTYRE, NCMILLS RIVER NEAR MILLS RIVER, NCBEETREE CREEK NEAR SWANNANOA, NCSWANNANOA RIVER AT BILTMORE, NCFRENCH BROAD RIVER AT ASHEVILLE, NCFRENCH BROAD RIVER NEAR NEWPORT, TN

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 FRENCH BROAD RIVER AT ASHEVILLE, NC
The highest instantaneous discharge the publisher recorded in each year — a flood peak as measured, not a daily average of one. 1810–2025.
Shading marks when something was recorded, not what caused the line.
Largest measured flow of each year at FRENCH BROAD RIVER AT ASHEVILLE, NCLargest measured flow of each year at FRENCH BROAD RIVER AT ASHEVILLE, NC: FRENCH BROAD RIVER AT ASHEVILLE, NC in m³/s, from 1810 to 2025.Hurricane Katrina water and sanitation collapse01,0002,0003,0004,000m³/s18101902192019421959197719952013

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
PeriodFRENCH BROAD RIVER AT ASHEVILLE, NC (m³/s)
18100
18450
18500
18520
18750
18760
18790
18920
18930
1896612
1897354
1898394
1899753
1900422
1901830
1902960
1903538
1904391
1905651
1906731
1908470
1909544
1910858
1911422
1912450
1913600
1914306
19163,115
1917391
1918345
1920538
1922281
1923377
1924272
1926292
19281,209
1929428
1931199
1932192
1934326
1935479
1936467
1937360
1939331
1940985
1942592
1944258
1945212
1946453
1947385
1948270
1949569
1950368
1952442
1953416
1954467
1955233
1956294
1957685
1958256
1959348
1960292
1961538
1963498
1964348
1966552
1967498
1968436
1969189
1970201
1972544
1973858
1974402
1975595
1976597
1977541
1979660
1981186
1982430
1983487
1984411
1985217
1987402
1988208
1989254
1990515
1991487
1992311
1993374
1994597
1995790
1996300
1998697
1999157
2000289
2001159
2002159
2003416
20041,220
2005345
2007274
2008230
2009470
2010371
2011276
2013657
2014274
2015569
2017269
2018592
2019739
2020476
2021736
2022194
20243,200
2025294

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 held1810–2025
Completeness53.7% of the periods in that span are held. Gaps are drawn as breaks and never interpolated.
Known gaps
  • 30 separate periods inside 1810–2025 hold no value. The longest runs from 1811 to 1844 — 34 years with no reading. They are drawn as breaks in the line and are never interpolated across.
ContinuityThe record begins in 1810 and is not continuous from it: 216 years separate the first value from the last, and 54% 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 FRENCH BROAD RIVER AT ASHEVILLE, NC, as a depth
The year's flow spread over the land draining to this gauge, in millimetres — the same unit rainfall is measured in. 1896–2025.
Shading marks when something was recorded, not what caused the line.
Water leaving the catchment above FRENCH BROAD RIVER AT ASHEVILLE, NC, as a depthWater leaving the catchment above FRENCH BROAD RIVER AT ASHEVILLE, NC, as a depth: FRENCH BROAD RIVER AT ASHEVILLE, NC in mm, from 1896 to 2025.Hurricane Katrina water and sanitation collapse5001,0001,500mm18961913193019471964198119982015

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
PeriodFRENCH BROAD RIVER AT ASHEVILLE, NC (mm)
1896561
1897714
1898834
18991,026
1900969
19011,412
1902795
1903991
1904427
1905764
19061,237
1907616
1908882
1909989
1910710
1911587
1912770
1913775
1914698
19151,021
19161,121
1917675
1918882
1919836
1920890
1921781
1922760
1923714
1924750
1925418
1926506
1927537
1928938
19291,045
1930463
1931494
1932816
1933669
1934711
1935686
1936953
1937843
1938567
1939661
1940639
1941460
1942767
1943768
1944613
1945605
1946818
1947616
1948814
19491,123
1950785
1951574
1952685
1953580
1954501
1955503
1956462
1957825
1958701
1959771
1960772
1961893
1962773
1963528
19641,023
1965729
1966692
1967791
1968664
1969840
1970588
1971754
1972795
19731,104
1974925
19751,049
1976850
1977845
1978716
19791,263
1980736
1981370
1982671
1983932
1984840
1985536
1986463
1987643
1988350
1989915
1990927
1991857
19921,003
1993763
1994937
19951,006
1996905
1997838
1998925
1999501
2000458
2001412
2002485
2003996
20041,055
2005931
2006606
2007440
2008382
2009803
2010764
2011636
2012581
20131,254
2014665
2015757
2016619
2017656
20181,285
20191,127
20201,245
2021888
2022721
2023520
2024938
2025612

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 held1896–2025
Completeness100.0% of the periods in that span are held.
ContinuityContinuous: every year from 1896 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 Upper French Broad and what each holds
GaugeMeasuresValuesRecord
FRENCH BROAD RIVER AT ASHEVILLE, NCburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year4361810–2026
FRENCH BROAD RIVER AT BLANTYRE, NCburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3611879–2026
FRENCH BROAD RIVER NEAR NEWPORT, TNburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3581867–2026
DAVIDSON RIVER NEAR BREVARD, NCburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3431916–2026
SWANNANOA RIVER AT BILTMORE, NCburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3321876–2026
MILLS RIVER NEAR MILLS RIVER, NCburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3171906–2026
FRENCH BROAD RIVER AT ROSMAN, NCburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3111907–2026
BEETREE CREEK NEAR SWANNANOA, NCburned area within 50 km, catchment area, annual maximum river flow, mean river flow, mean river flow, water year3091926–2026

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 — 06010105. 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
FRENCH BROAD RIVER AT ASHEVILLE, NCStated 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
FRENCH BROAD RIVER AT BLANTYRE, NCStated 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
FRENCH BROAD RIVER NEAR NEWPORT, TNStated 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
DAVIDSON RIVER NEAR BREVARD, NCStated 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
SWANNANOA RIVER AT BILTMORE, NCStated 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
MILLS RIVER NEAR MILLS RIVER, NCStated 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
FRENCH BROAD RIVER AT ROSMAN, NCStated 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
BEETREE CREEK NEAR SWANNANOA, NCStated 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 record8yes, 3 or more
Years spanned217yes, 20 or more
Values held2,767yes, 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), Upper French Broad gauge records, accessed 2026-10-05, hydrionis.com/waters/united-states-upper-french-broad/

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 Upper French Broad 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 confidence2025-02-13

Source: USGS — National Water Information System, USGS site 03451500, 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.