Torne river
Also known as: Torneälven, Tornelven, Tornio, Tornionjoki
The Torne (also known as Torneälven, Tornelven, Tornio, Tornionjoki) is a European river flowing through Sweden, Finland. As of 2026-10-14, the Torne was flowing at about 370.2 m³/s at the Pello gauge.
- Canonical name
- Torne
- Local names / aliases
- Torneälven, Tornelven, Tornio, Tornionjoki
- Countries
- Sweden, Finland
- Maximum upstream drainage area
- 38,614 km²
- Mapped river length
- 355.9 km
- Gauging stations
- 4
- Classification
- Major European river
- Latest measured discharge
- 370.2 m³/s (Pello, 2026-10-14)
Gauging stations on the Torne
The following 4 gauging stations report discharge for the Torne, ordered downstream (largest catchment first). Discharge is in cubic metres per second (m³/s).
| Station | Country | Discharge (m³/s) | Historical Comparison | Observed | Measurement | Data quality | Provider | Lat, Lon | Source |
|---|---|---|---|---|---|---|---|---|---|
| Pello | Finland | 370.2 | Normal17% above the historic median | daily mean | SYKE flag 108 | Finnish Environment Institute | 66.785, 23.916 | source | |
| PAJALA PUMPHUS | Sweden | 137 | Much above normal108% above the historic median | instantaneous | SMHI quality O | Swedish Meteorological and Hydrological Institute | 67.207, 23.396 | source | |
| JUNOSUANDO | Sweden | 61 | Above normal106% above the historic median | instantaneous | SMHI quality O | Swedish Meteorological and Hydrological Institute | 67.428, 22.546 | source | |
| ABISKO | Sweden | 67.7 | Much above normal57% above the historic median | instantaneous | SMHI quality O | Swedish Meteorological and Hydrological Institute | 68.194, 19.986 | source |
Related rivers
- Gta lv
- Ångermanälven
- Dalälven
- Indalsälven
- Luleälven
- Stora Luleälven
- Kalixälven
- Umeälven
- Motala ström
- Skellefteälven
- Kalix
- Piteälven
Data, sources & timestamps
Geometry is the HydroRIVERS network (HydroSHEDS): European reaches with at least 500 km² of upstream catchment, merged into chains between confluences. Flow direction comes from the network itself; river names are the canonical English label joined from provider metadata and Natural Earth, with local-language aliases retained.
Discharge is normalised observed streamflow from official national hydrology providers, measured where a gauge sits on the river and interpolated between gauges. Pale/estimated values are derived from drainage area × the local specific discharge of nearby gauges and are never presented as measurements.