The monitoring network within this area

Hydrionis holds 22,518 values from 2 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.

2
Gauges
22,518
Values held
1967–2026
Record spans
2,312 km²
Area
Gauges within the Gavleån drainage basin
2 monitoring points, positioned as the publisher records them.
Gauges within the Gavleån drainage basinLumsheden-Midge VM, TOLVFORS KRVLumsheden-Midge VMTOLVFORS KRV

How low, how high and how variable this gauge runs

A hydrograph says what happened; these say how often. Read off TOLVFORS KRV's whole daily record between 1967 and 2026, 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.

2.000 m³/s
Q95 low flow
14.300 m³/s
Q50 median flow
35.200 m³/s
Q10 high flow
Largest day of each water year at TOLVFORS KRV
The highest daily mean discharge in each October-to-September water year, 1967–2025.
Largest day of each water year at TOLVFORS KRVLargest day of each water year at TOLVFORS KRV: TOLVFORS KRV in m³/s, from 1967 to 2025.050100150200m³/s19671975198319911999200720152023TOLVFORS KRV 1967: 44.0 m³/sTOLVFORS KRV 1968: 106 m³/sTOLVFORS KRV 1969: 108 m³/sTOLVFORS KRV 1970: 42.0 m³/sTOLVFORS KRV 1971: 40.0 m³/sTOLVFORS KRV 1972: 28.0 m³/sTOLVFORS KRV 1973: 25.0 m³/sTOLVFORS KRV 1974: 114 m³/sTOLVFORS KRV 1975: 13.0 m³/sTOLVFORS KRV 1976: 152 m³/sTOLVFORS KRV 1977: 46.0 m³/sTOLVFORS KRV 1978: 95.0 m³/sTOLVFORS KRV 1979: 38.0 m³/sTOLVFORS KRV 1980: 90.0 m³/sTOLVFORS KRV 1981: 98.0 m³/sTOLVFORS KRV 1982: 79.0 m³/sTOLVFORS KRV 1983: 74.0 m³/sTOLVFORS KRV 1984: 150 m³/sTOLVFORS KRV 1985: 169 m³/sTOLVFORS KRV 1986: 51.0 m³/sTOLVFORS KRV 1987: 93.0 m³/sTOLVFORS KRV 1988: 62.0 m³/sTOLVFORS KRV 1989: 51.0 m³/sTOLVFORS KRV 1990: 61.0 m³/sTOLVFORS KRV 1991: 67.0 m³/sTOLVFORS KRV 1992: 90.0 m³/sTOLVFORS KRV 1993: 62.0 m³/sTOLVFORS KRV 1994: 126 m³/sTOLVFORS KRV 1995: 29.0 m³/sTOLVFORS KRV 1996: 36.4 m³/sTOLVFORS KRV 1997: 36.9 m³/sTOLVFORS KRV 1998: 112 m³/sTOLVFORS KRV 1999: 84.0 m³/sTOLVFORS KRV 2000: 106 m³/sTOLVFORS KRV 2001: 75.8 m³/sTOLVFORS KRV 2002: 65.5 m³/sTOLVFORS KRV 2003: 43.3 m³/sTOLVFORS KRV 2004: 34.7 m³/sTOLVFORS KRV 2005: 63.6 m³/sTOLVFORS KRV 2006: 95.7 m³/sTOLVFORS KRV 2007: 48.6 m³/sTOLVFORS KRV 2008: 79.8 m³/sTOLVFORS KRV 2009: 56.4 m³/sTOLVFORS KRV 2010: 96.3 m³/sTOLVFORS KRV 2011: 56.5 m³/sTOLVFORS KRV 2012: 79.1 m³/sTOLVFORS KRV 2013: 29.6 m³/sTOLVFORS KRV 2014: 57.1 m³/sTOLVFORS KRV 2015: 49.1 m³/sTOLVFORS KRV 2016: 43.2 m³/sTOLVFORS KRV 2017: 127 m³/sTOLVFORS KRV 2018: 80.5 m³/sTOLVFORS KRV 2019: 97.3 m³/sTOLVFORS KRV 2020: 129 m³/sTOLVFORS KRV 2021: 62.7 m³/sTOLVFORS KRV 2022: 156 m³/sTOLVFORS KRV 2023: 114 m³/sTOLVFORS KRV 2024: 36.5 m³/sTOLVFORS KRV 2025: 56.6 m³/s

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
PeriodTOLVFORS KRV (m³/s)
196744.0
1968106
1969108
197042.0
197140.0
197228.0
197325.0
1974114
197513.0
1976152
197746.0
197895.0
197938.0
198090.0
198198.0
198279.0
198374.0
1984150
1985169
198651.0
198793.0
198862.0
198951.0
199061.0
199167.0
199290.0
199362.0
1994126
199529.0
199636.4
199736.9
1998112
199984.0
2000106
200175.8
200265.5
200343.3
200434.7
200563.6
200695.7
200748.6
200879.8
200956.4
201096.3
201156.5
201279.1
201329.6
201457.1
201549.1
201643.2
2017127
201880.5
201997.3
2020129
202162.7
2022156
2023114
202436.5
202556.6

The longest record here

Mean river flow at TOLVFORS KRV
Annual means of the daily record, 1967–2025. One gauge, not this drainage area.
Mean river flow at TOLVFORS KRVMean river flow at TOLVFORS KRV: TOLVFORS KRV in m³/s, from 1967 to 2025.010203040m³/s19671975198319911999200720152023TOLVFORS KRV 1967: 27.7 m³/sTOLVFORS KRV 1968: 17.0 m³/sTOLVFORS KRV 1969: 21.4 m³/sTOLVFORS KRV 1970: 17.6 m³/sTOLVFORS KRV 1971: 15.0 m³/sTOLVFORS KRV 1972: 12.4 m³/sTOLVFORS KRV 1973: 11.5 m³/sTOLVFORS KRV 1974: 21.5 m³/sTOLVFORS KRV 1975: 14.0 m³/sTOLVFORS KRV 1976: 8.05 m³/sTOLVFORS KRV 1977: 29.6 m³/sTOLVFORS KRV 1978: 17.5 m³/sTOLVFORS KRV 1979: 17.8 m³/sTOLVFORS KRV 1980: 17.9 m³/sTOLVFORS KRV 1981: 27.8 m³/sTOLVFORS KRV 1982: 23.4 m³/sTOLVFORS KRV 1983: 22.9 m³/sTOLVFORS KRV 1984: 23.2 m³/sTOLVFORS KRV 1985: 27.8 m³/sTOLVFORS KRV 1986: 29.0 m³/sTOLVFORS KRV 1987: 22.9 m³/sTOLVFORS KRV 1988: 19.9 m³/sTOLVFORS KRV 1989: 13.2 m³/sTOLVFORS KRV 1990: 18.2 m³/sTOLVFORS KRV 1991: 18.9 m³/sTOLVFORS KRV 1992: 15.4 m³/sTOLVFORS KRV 1993: 14.2 m³/sTOLVFORS KRV 1994: 17.0 m³/sTOLVFORS KRV 1995: 24.8 m³/sTOLVFORS KRV 1996: 9.61 m³/sTOLVFORS KRV 1997: 12.8 m³/sTOLVFORS KRV 1998: 22.5 m³/sTOLVFORS KRV 1999: 21.9 m³/sTOLVFORS KRV 2000: 27.3 m³/sTOLVFORS KRV 2001: 20.6 m³/sTOLVFORS KRV 2002: 19.0 m³/sTOLVFORS KRV 2003: 16.4 m³/sTOLVFORS KRV 2004: 16.5 m³/sTOLVFORS KRV 2005: 12.5 m³/sTOLVFORS KRV 2006: 23.8 m³/sTOLVFORS KRV 2007: 12.7 m³/sTOLVFORS KRV 2008: 19.7 m³/sTOLVFORS KRV 2009: 22.3 m³/sTOLVFORS KRV 2010: 18.5 m³/sTOLVFORS KRV 2011: 15.8 m³/sTOLVFORS KRV 2012: 23.4 m³/sTOLVFORS KRV 2013: 11.2 m³/sTOLVFORS KRV 2014: 11.5 m³/sTOLVFORS KRV 2015: 14.9 m³/sTOLVFORS KRV 2016: 14.9 m³/sTOLVFORS KRV 2017: 14.6 m³/sTOLVFORS KRV 2018: 19.6 m³/sTOLVFORS KRV 2019: 21.6 m³/sTOLVFORS KRV 2020: 16.7 m³/sTOLVFORS KRV 2021: 25.7 m³/sTOLVFORS KRV 2022: 9.81 m³/sTOLVFORS KRV 2023: 34.6 m³/sTOLVFORS KRV 2024: 18.5 m³/sTOLVFORS KRV 2025: 16.7 m³/s

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
PeriodTOLVFORS KRV (m³/s)
196727.7
196817.0
196921.4
197017.6
197115.0
197212.4
197311.5
197421.5
197514.0
19768.05
197729.6
197817.5
197917.8
198017.9
198127.8
198223.4
198322.9
198423.2
198527.8
198629.0
198722.9
198819.9
198913.2
199018.2
199118.9
199215.4
199314.2
199417.0
199524.8
19969.61
199712.8
199822.5
199921.9
200027.3
200120.6
200219.0
200316.4
200416.5
200512.5
200623.8
200712.7
200819.7
200922.3
201018.5
201115.8
201223.4
201311.2
201411.5
201514.9
201614.9
201714.6
201819.6
201921.6
202016.7
202125.7
20229.81
202334.6
202418.5
202516.7

Every gauge Hydrionis holds within this area

Gauges within the Gavleån and what each holds
GaugeMeasuresValuesRecord
TOLVFORS KRVmean river flow21,8171967–2026
Lumsheden-Midge VMmean river flow7012013–2016

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 — 52000. 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
TOLVFORS KRVStated by the publisher on the record this gauge’s observations came from.With the observations
Lumsheden-Midge VMStated 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 2 of them, which makes it a profile, not indexed.

Information-gain signals held for this water body
SignalHeldCounts
Gauges holding a real record2no
Years spanned60yes, 20 or more
Values held22,518yes, 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), Gavleån gauge records, accessed 2026-10-05, hydrionis.com/waters/sweden-gavlean/

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 Gavleån 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 confidence2026-09-30

Source: SMHI — Swedish hydrological observations, 1940. 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 2002-12-31 to 2002-12-31 (not yet checked), 2026-01-18 to 2026-09-30 (not yet checked). Station in the GAVLEÅN main drainage basin, 2,312 km². Discharge is a property of this gauge and this reach, not of the river as a whole.

Retrieved 1 October 2026.