The monitoring network within this area

Hydrionis holds 485,971 values from 30 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.

30
Gauges
485,971
Values held
1909–2026
Record spans
26,568 km²
Area
Gauges within the Umeälven drainage basin
30 monitoring points, positioned as the publisher records them.
Gauges within the Umeälven drainage basinBERGLUNDA, BJURÅKER, BJÖRKSELE, DEGERFORS ÖVRE, DEGERFORS, FRÄKENVIK, GAUTRÄSK, GRANSELET 2, GRANÅKER, HARRSELE KRV, HÄLLBACKEN, JUKTNÄS, KARLSTEN, LAISVALL, NEDRE JOVATTNET, PENGFORS, SANDNÄSUDDEN, SKIRKNÄS, SLUSSFORS, SLÄTVIK, SOLBERG 2, SOLBERG, SORSELE 2, SORSELE, STORJUKTAN TOTALT, STORNORRFORS KRV, STORUMAN 2, TÄNGVATTNET, UMASJÖ, VÄNNÄSBERGLUNDABJURÅKERBJÖRKSELEDEGERFORS ÖVREDEGERFORSFRÄKENVIKGAUTRÄSKGRANSELET 2GRANÅKERHARRSELE KRVHÄLLBACKENJUKTNÄSKARLSTENLAISVALLNEDRE JOVATTNETPENGFORSSANDNÄSUDDENSKIRKNÄSSLUSSFORSSLÄTVIKSOLBERG 2SOLBERGSORSELE 2SORSELESTORJUKTAN TOTALTSTORNORRFORS KRVSTORUMAN 2TÄNGVATTNETUMASJÖVÄNNÄS

How low, how high and how variable this gauge runs

A hydrograph says what happened; these say how often. Read off SOLBERG's whole daily record between 1911 and 2019, they describe the shape of the record rather than any day in it — and they belong to this gauge and its reach, not to this drainage area.

2.030 m³/s
Q95 low flow
11.800 m³/s
Q50 median flow
79.100 m³/s
Q10 high flow
Largest day of each water year at SOLBERG
The highest daily mean discharge in each October-to-September water year, 1911–2017.
Largest day of each water year at SOLBERGLargest day of each water year at SOLBERG: SOLBERG in m³/s, from 1911 to 2017.200400600m³/s19111925193919531967198119952009

These are the largest daily means, not flood peaks. A peak lasting hours is averaged across a whole day here, so the true instantaneous maximum on the same day was higher — sometimes far higher on a fast-responding catchment. Flood frequency work needs a publisher's own instantaneous series; Hydrionis holds one for 2,236 American gauges and not for this one, so the two are never drawn together. A water year the gauge did not substantially cover produces no value at all rather than a low one.

View the data behind this chart
Underlying data
PeriodSOLBERG (m³/s)
1911111
1912220
1913255
1914196
1915177
1916246
1917164
1918129
1919255
1920254
1921263
1922147
1923230
1924244
1925244
1926244
1927105
1928237
1929274
1930133
1931160
1932190
1933270
1934261
1935169
1936138
1937340
1938267
1939191
1940186
1941183
1942328
1943220
1944230
1945211
1946119
1947204
1948296
1949296
1950186
1951214
1952294
1953199
1954175
1955223
1956203
1957235
1958194
1959209
1960308
1961127
1962244
1963164
1964185
1965201
1966312
1967274
1968135
1969204
1970326
1971259
1972286
1973180
1974241
1975267
1976243
1977230
1978241
1979292
1980274
1981235
1982220
1983288
1984198
1985169
1986186
1987209
1988214
1989198
1990194
1991265
1992263
1993166
1994512
1995174
1996308
1997203
1998163
1999210
2000145
2001177
2002200
2003253
2004360
2005129
2006149
2007157
2008123
2009305
2010263
2011187
2012339
2013251
2014187
2015186
2016247
2017321

The longest record here

Mean river flow at SOLBERG
Annual means of the daily record, 1911–2018. One gauge, not this drainage area.
Mean river flow at SOLBERGMean river flow at SOLBERG: SOLBERG in m³/s, from 1911 to 2018.203040m³/s19111925193919531967198119952009

Annual means computed by Hydrionis from the published daily record, drawn only for years with at least 300 days held. They summarise this gauge's own record and say nothing about any other watercourse in this area.

View the data behind this chart
Underlying data
PeriodSOLBERG (m³/s)
191123.5
191217.7
191326.7
191429.6
191523.7
191620.8
191726.3
191829.2
191931.0
192036.9
192135.5
192232.1
192327.7
192429.1
192534.8
192626.1
192731.3
192821.6
192931.5
193031.4
193127.8
193231.1
193325.5
193436.3
193527.7
193626.3
193724.0
193834.1
193924.1
194026.0
194126.9
194227.2
194338.9
194429.2
194530.2
194629.0
194720.2
194831.8
194942.2
195031.8
195122.5
195226.3
195339.2
195425.1
195523.0
195623.2
195729.0
195833.1
195925.5
196022.7
196136.3
196223.0
196327.7
196430.5
196525.7
196627.3
196728.9
196823.8
196918.9
197021.8
197130.6
197233.2
197333.8
197428.1
197530.6
197628.0
197726.3
197828.3
197927.7
198021.1
198126.4
198227.7
198332.6
198433.9
198532.3
198625.7
198731.2
198828.6
198940.7
199039.4
199132.2
199234.0
199341.3
199422.5
199537.5
199622.4
199737.0
199838.8
199926.8
200034.3
200134.6
200230.5
200325.3
200433.8
200533.3
200621.0
200723.0
200819.5
200921.8
201025.3
201137.1
201229.8
201322.6
201424.8
201535.7
201624.0
201730.6
201829.2

Every gauge Hydrionis holds within this area

Gauges within the Umeälven and what each holds
GaugeMeasuresValuesRecord
SOLBERGmean river flow39,6801911–2019
HÄLLBACKENmean river flow29,2501910–1990
KARLSTENmean river flow29,1481919–1999
SORSELEmean river flow25,5271909–1979
TÄNGVATTNETmean river flow25,4441957–2026
SLÄTVIKmean river flow25,3421911–1980
STORNORRFORS KRVmean river flow24,8661958–2026
STORUMAN 2mean river flow24,8661958–2026
HARRSELE KRVmean river flow24,7761958–2026
GAUTRÄSKmean river flow23,2761953–2026
FRÄKENVIKmean river flow18,6101910–1961
SORSELE 2mean river flow17,2901979–2026
STORJUKTAN TOTALTmean river flow17,2551978–2026
GRANÅKERmean river flow17,2271979–2026
SKIRKNÄSmean river flow16,9351980–2026
NEDRE JOVATTNETmean river flow16,4371956–2000
JUKTNÄSmean river flow15,7051917–1959
UMASJÖmean river flow13,8211910–1948
LAISVALLmean river flow13,6031989–2026
SANDNÄSUDDENmean river flow13,2411919–1955
DEGERFORSmean river flow10,2271911–1938
GRANSELET 2mean river flow7,8911979–2001
SLUSSFORSmean river flow7,6721910–1931
BERGLUNDAmean river flow6,6651923–1957
BJURÅKERmean river flow4,7331919–1931
PENGFORSmean river flow4,4751920–1932
DEGERFORS ÖVREmean river flow4,2631938–1949
VÄNNÄSmean river flow3,2851910–1922
SOLBERG 2mean river flow2,6342019–2026
BJÖRKSELEmean river flow1,8271910–1916

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 — 28000. 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
SOLBERGStated by the publisher on the record this gauge’s observations came from.With the observations
HÄLLBACKENStated by the publisher on the record this gauge’s observations came from.With the observations
KARLSTENStated by the publisher on the record this gauge’s observations came from.With the observations
SORSELEStated by the publisher on the record this gauge’s observations came from.With the observations
TÄNGVATTNETStated by the publisher on the record this gauge’s observations came from.With the observations
SLÄTVIKStated by the publisher on the record this gauge’s observations came from.With the observations
STORNORRFORS KRVStated by the publisher on the record this gauge’s observations came from.With the observations
STORUMAN 2Stated by the publisher on the record this gauge’s observations came from.With the observations
HARRSELE KRVStated by the publisher on the record this gauge’s observations came from.With the observations
GAUTRÄSKStated by the publisher on the record this gauge’s observations came from.With the observations
FRÄKENVIKStated by the publisher on the record this gauge’s observations came from.With the observations
SORSELE 2Stated by the publisher on the record this gauge’s observations came from.With the observations
STORJUKTAN TOTALTStated by the publisher on the record this gauge’s observations came from.With the observations
GRANÅKERStated by the publisher on the record this gauge’s observations came from.With the observations
SKIRKNÄSStated by the publisher on the record this gauge’s observations came from.With the observations
NEDRE JOVATTNETStated by the publisher on the record this gauge’s observations came from.With the observations
JUKTNÄSStated by the publisher on the record this gauge’s observations came from.With the observations
UMASJÖStated by the publisher on the record this gauge’s observations came from.With the observations
LAISVALLStated by the publisher on the record this gauge’s observations came from.With the observations
SANDNÄSUDDENStated by the publisher on the record this gauge’s observations came from.With the observations
DEGERFORSStated by the publisher on the record this gauge’s observations came from.With the observations
GRANSELET 2Stated by the publisher on the record this gauge’s observations came from.With the observations
SLUSSFORSStated by the publisher on the record this gauge’s observations came from.With the observations
BERGLUNDAStated by the publisher on the record this gauge’s observations came from.With the observations
BJURÅKERStated by the publisher on the record this gauge’s observations came from.With the observations
PENGFORSStated by the publisher on the record this gauge’s observations came from.With the observations
DEGERFORS ÖVREStated by the publisher on the record this gauge’s observations came from.With the observations
VÄNNÄSStated by the publisher on the record this gauge’s observations came from.With the observations
SOLBERG 2Stated by the publisher on the record this gauge’s observations came from.With the observations
BJÖRKSELEStated by the publisher on the record this gauge’s observations came from.With the observations

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 record30yes, 3 or more
Years spanned118yes, 20 or more
Values held485,971yes, 1000 or more
Distinct measurements1no
Publishers measuring it1no
Official identifiers2recorded, 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

Attribution you are required to give

These are conditions of the licences the underlying data is published under. They are obligations to the publishers, not to Hydrionis, and they apply to you directly whether or not you mention Hydrionis at all.

Data from Sveriges meteorologiska och hydrologiska institut, used under CC BY 4.0.

Suggested citation for Hydrionis

Hydrionis (2026), Umeälven gauge records, accessed 2026-10-05, hydrionis.com/waters/sweden-umealven/

Cite Hydrionis where you rely on the compilation, the normalisation, the eligibility judgements or a chart. Where you use an unmodified published value, the publisher’s attribution is the one that is required; crediting Hydrionis as well is welcome and is not something Hydrionis can require of you.

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 Umeälven 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.

Where these figures come from

MeasuredMedium confidence2019-09-30

Source: SMHI — Swedish hydrological observations, 436. Licence: Open — attribution required (attribution required).

Method: Daily discharge exactly as SMHI publishes it, from its corrected archive. SMHI computes the daily value from its own sub-daily measurement and rating curves; Hydrionis does not recompute it, because a mean derived from whatever sub-daily data happens to be exposed would be a different statistic under the same name.

Checked and approved by SMHI except 2019-06-11 to 2019-09-30 (not yet checked). Station in the UMEÄLVEN main drainage basin, 1,084 km². Discharge is a property of this gauge and this reach, not of the river as a whole.

Retrieved 1 October 2026.