Sweden Historical River Discharge Dataset
Daily river discharge for the Swedish national hydrological network, from 1851 to the present: 694 gauging stations across 87 main drainage basins, taken exactly as SMHI publishes it. The deepest openly licensed daily river record Hydrionis holds.
What this looks like
One real series from the dataset, and real rows from the head of its published extract. Neither is a mock-up: the rows below are the same rows, unchanged, that are in the file you would download.
Drawn to show the shape and resolution of what the dataset contains, not to make a point about ÖVRE HYNDEVAD. Gaps are breaks, never interpolated.
View the data behind this chart
| Period | ÖVRE HYNDEVAD (m³/s) |
|---|---|
| 1889 | 27.0 |
| 1890 | 17.0 |
| 1891 | 20.0 |
| 1892 | 21.0 |
| 1893 | 12.0 |
| 1894 | 22.0 |
| 1895 | 47.0 |
| 1896 | 18.0 |
| 1897 | 30.0 |
| 1898 | 38.0 |
| 1899 | 70.0 |
| 1900 | 11.0 |
| 1901 | 20.0 |
| 1902 | 7.90 |
| 1903 | 15.0 |
| 1904 | 38.0 |
| 1905 | 9.80 |
| 1906 | 21.0 |
| 1907 | 14.0 |
| 1908 | 18.0 |
| 1909 | 11.0 |
| 1910 | 89.0 |
| 1911 | 48.0 |
| 1912 | 22.0 |
| 1913 | 54.0 |
| 1914 | 19.0 |
| 1915 | 10.0 |
| 1916 | 21.0 |
| 1917 | 41.0 |
| 1918 | 20.0 |
| 1919 | 22.0 |
| 1920 | 4.40 |
| 1921 | 10.0 |
| 1922 | 3.00 |
| 1923 | 3.70 |
| 1924 | 57.0 |
| 1925 | 24.0 |
| 1926 | 4.10 |
| 1927 | 22.0 |
| 1928 | 6.50 |
| 1929 | 22.0 |
| 1930 | 25.0 |
| 1931 | 26.0 |
| 1932 | 10.0 |
| 1933 | 6.90 |
| 1934 | 3.00 |
| 1935 | 71.0 |
| 1936 | 26.0 |
| 1937 | 8.50 |
| 1938 | 20.0 |
| 1939 | 102 |
| 1940 | 14.3 |
| 1941 | 17.0 |
| 1942 | 8.80 |
| 1943 | 16.3 |
| 1944 | 20.0 |
| 1945 | 80.0 |
| 1946 | 10.3 |
| 1947 | 22.0 |
| 1948 | 3.30 |
| 1949 | 7.20 |
| 1950 | 69.0 |
| 1951 | 37.0 |
| 1952 | 41.0 |
| 1953 | 34.0 |
| 1954 | 20.0 |
| 1955 | 67.0 |
| 1956 | 32.0 |
| 1957 | 24.0 |
| 1958 | 25.0 |
| 1959 | 52.0 |
| 1960 | 22.0 |
| 1961 | 58.0 |
| 1962 | 31.0 |
| 1963 | 22.0 |
| 1964 | 21.0 |
| 1965 | 27.0 |
| 1966 | 25.0 |
| 1967 | 82.0 |
| 1968 | 23.0 |
| 1969 | 30.0 |
| 1970 | 8.80 |
| 1971 | 28.0 |
| 1972 | 26.0 |
| 1973 | 29.0 |
| 1974 | 10.6 |
| 1975 | 74.0 |
| 1976 | 7.00 |
| 1977 | 22.0 |
| 1978 | 27.0 |
| 1979 | 12.2 |
| 1980 | 27.0 |
| 1981 | 33.0 |
| 1982 | 62.0 |
| 1983 | 43.0 |
| 1984 | 37.0 |
| 1985 | 30.0 |
| 1986 | 48.0 |
| 1987 | 26.0 |
| 1988 | 79.0 |
| 1989 | 42.0 |
| 1990 | 53.0 |
| 1991 | 26.0 |
| 1992 | 12.6 |
| 1993 | 22.0 |
| 1994 | 48.0 |
| 1995 | 18.4 |
| 1996 | 4.30 |
| 1997 | 24.5 |
| 1998 | 33.4 |
| 1999 | 32.7 |
| 2000 | 27.6 |
| 2001 | 64.8 |
| 2002 | 53.0 |
| 2003 | 3.10 |
| 2004 | 27.0 |
| 2005 | 23.1 |
| 2006 | 20.2 |
| 2007 | 58.0 |
| 2008 | 64.5 |
| 2009 | 38.0 |
| 2010 | 53.0 |
| 2011 | 31.5 |
| 2012 | 38.0 |
| 2013 | 38.0 |
| 2014 | 38.5 |
| 2015 | 22.0 |
| 2016 | 29.7 |
| 2017 | 3.30 |
| 2018 | 42.7 |
| 2019 | 10.0 |
| 2020 | 46.0 |
| 2021 | 16.0 |
| 2022 | 6.60 |
| 2023 | 59.1 |
| 2024 | 90.0 |
| 2025 | 65.7 |
| 2026 | 60.0 |
Sample rows
metric_id | subject_id | subject_kind | value | censored | censor_operator | censor_threshold | censor_limit | censor_reported | unit | period_start | period_end | period_kind | basis | confidence | source_id | source_ref | qualifier | superseded | retrieved |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| river-flow-mean | se-smhi-10 | geography | 6 | — | — | — | — | — | m³/s | 1917-01-01 | 1917-01-01 | day | measured | high | se-smhi-hydro | 10 | — | — | 2026-10-01 |
| river-flow-mean | se-smhi-10 | geography | 5.9 | — | — | — | — | — | m³/s | 1917-01-02 | 1917-01-02 | day | measured | high | se-smhi-hydro | 10 | — | — | 2026-10-01 |
| river-flow-mean | se-smhi-10 | geography | 5.9 | — | — | — | — | — | m³/s | 1917-01-03 | 1917-01-03 | day | measured | high | se-smhi-hydro | 10 | — | — | 2026-10-01 |
| river-flow-mean | se-smhi-10 | geography | 5.8 | — | — | — | — | — | m³/s | 1917-01-04 | 1917-01-04 | day | measured | high | se-smhi-hydro | 10 | — | — | 2026-10-01 |
| river-flow-mean | se-smhi-10 | geography | 5.7 | — | — | — | — | — | m³/s | 1917-01-05 | 1917-01-05 | day | measured | high | se-smhi-hydro | 10 | — | — | 2026-10-01 |
| river-flow-mean | se-smhi-10 | geography | 5.7 | — | — | — | — | — | m³/s | 1917-01-06 | 1917-01-06 | day | measured | high | se-smhi-hydro | 10 | — | — | 2026-10-01 |
| river-flow-mean | se-smhi-10 | geography | 5.6 | — | — | — | — | — | m³/s | 1917-01-07 | 1917-01-07 | day | measured | high | se-smhi-hydro | 10 | — | — | 2026-10-01 |
| river-flow-mean | se-smhi-10 | geography | 5.5 | — | — | — | — | — | m³/s | 1917-01-08 | 1917-01-08 | day | measured | high | se-smhi-hydro | 10 | — | — | 2026-10-01 |
| river-flow-mean | se-smhi-10 | geography | 5.5 | — | — | — | — | — | m³/s | 1917-01-09 | 1917-01-09 | day | measured | high | se-smhi-hydro | 10 | — | — | 2026-10-01 |
| river-flow-mean | se-smhi-10 | geography | 5.4 | — | — | — | — | — | m³/s | 1917-01-10 | 1917-01-10 | day | measured | high | se-smhi-hydro | 10 | — | — | 2026-10-01 |
| river-flow-mean | se-smhi-10 | geography | 5.4 | — | — | — | — | — | m³/s | 1917-01-11 | 1917-01-11 | day | measured | high | se-smhi-hydro | 10 | — | — | 2026-10-01 |
| river-flow-mean | se-smhi-10 | geography | 5.3 | — | — | — | — | — | m³/s | 1917-01-12 | 1917-01-12 | day | measured | high | se-smhi-hydro | 10 | — | — | 2026-10-01 |
Methodology
Collected from the SMHI open data hydrological service under CC BY 4.0. Values are stored as SMHI publishes them and are not recomputed: SMHI derives each daily discharge from its own sub-daily measurement and rating curves, and a mean recalculated by Hydrionis from whatever sub-daily data happened to be exposed would be a different statistic under the same name. SMHI marks every value checked-and-approved, roughly-checked or unchecked, and all three levels are stored — the roughly-checked periods sit inside continuous records rather than at their ends, so excluding them would leave silent gaps. Each series states which of its periods carry which level, and takes the weakest as its confidence. Values carrying an unrecognised quality code, or an empty cell, are refused rather than converted.
What this dataset cannot tell you
Coverage
| Subjects | Swedish hydrological gauging stations with a corrected archive — 694 held |
|---|---|
| Period | 1851–2026 |
| Units | m³/s |
| Update cadence | Daily |
| Identifier | sweden-river-discharge v1.0.0 |
Fields
Data dictionary →Every metric this dataset carries, with the unit it is stored in and the geography level it is reported at. Full definitions are in the data dictionary.
| Identifier | Field | Unit | Reported at |
|---|---|---|---|
river-flow-mean | Mean river flow | m³/s | river-gauge |
Rights and access
Licence position
Open with attribution. Derivative use true; redistribution true; commercial reuse true.
Permitted uses
- Public display
- Derived analysis
- API delivery
- Bulk download
- Commercial use
Available to: Public, Developer, Research, Professional, Enterprise. These follow from the rights of the contributing publishers, not from a Hydrionis pricing decision — no access tier can widen what a publisher withheld.
Contributing sources
Attribution and citation
Cite and reuse →Two different obligations, deliberately kept apart. One is a condition of somebody else's licence; the other is a request Hydrionis has no standing to enforce.
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), Sweden Historical River Discharge Dataset, version 1.0.0, accessed 2026-10-05, hydrionis.com/data/datasets/sweden-river-discharge/
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.
Changelog
Version 1.0.0 — 2026-08-25
First release. Sweden becomes the deepest river record on the platform.
Additions
- Daily discharge for 694 stations across 87 main drainage basins, 1851 onward.
- Catchment name, official basin number and basin area carried onto every station.
Use this data
Use this data
- Download river-flow observations from SMHI, part 1 of 10 (1,000,000 rows) (CSV)
- Download river-flow observations from SMHI, part 2 of 10 (1,000,000 rows) (CSV)
- Download river-flow observations from SMHI, part 3 of 10 (1,000,000 rows) (CSV)
- Download river-flow observations from SMHI, part 4 of 10 (1,000,000 rows) (CSV)
- Download river-flow observations from SMHI, part 5 of 10 (1,000,000 rows) (CSV)
- Download river-flow observations from SMHI, part 6 of 10 (1,000,000 rows) (CSV)
- Download river-flow observations from SMHI, part 7 of 10 (1,000,000 rows) (CSV)
- Download river-flow observations from SMHI, part 8 of 10 (1,000,000 rows) (CSV)
- Download river-flow observations from SMHI, part 9 of 10 (1,000,000 rows) (CSV)
- Download river-flow observations from SMHI, part 10 of 10 (563,204 rows) (CSV)
- Machine-readable JSON
/api/v1/datasets/sweden-river-discharge.json - How to cite this, and who you must credit
- How these figures were produced
- Request this at a different scale, format or geography
About this data
The fields a professional user needs to judge whether this is fit for a particular purpose. Deliberately not a score.
About this data
| Source | Sveriges meteorologiska och hydrologiska institut — Swedish hydrological observations · CC BY 4.0 |
|---|---|
| How the values came to exist | Mixed across the series — the basis is recorded on every individual value. |
| Period held | 1851–2026 |
| Known gaps |
|
| Continuity | Version 1.0.0, released 2026-08-25. 1 recorded version; breaking changes and corrections are listed in the changelog above. |
| Last read from the publisher | 2026-10-01 · publisher updates daily |
| Redistribution | Permitted by the upstream licences |
| Commercial reuse | Permitted by the upstream licences. No Hydrionis access tier can widen this. |
| Methodology | How this was produced |