Ipoly river
The Ipoly is a European river flowing through Hungary. As of 2026-10-09, the Ipoly was flowing at about 0.401 m³/s at the Ipolytölgyes gauge.
- Canonical name
- Ipoly
- Countries
- Hungary
- Maximum upstream drainage area
- 5,148 km²
- Mapped river length
- 139.8 km
- Gauging stations
- 4
- Latest measured discharge
- 0.401 m³/s (Ipolytölgyes, 2026-10-09)
Gauging stations on the Ipoly
The following 4 gauging stations report discharge for the Ipoly, 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 |
|---|---|---|---|---|---|---|---|---|---|
| Ipolytölgyes | Hungary | 0.401 | Much below normal92% below the historic median | instantaneous | operational open-data observation | Hungarian General Directorate of Water Management | 47.925, 18.765 | source | |
| Ipolytarnóc | Hungary | 0.336 | Much below normal79% below the historic median | instantaneous | operational open-data observation | Hungarian General Directorate of Water Management | 48.236, 19.606 | source | |
| Nógrádszakál | Hungary | 0.37 | Much below normal86% below the historic median | instantaneous | operational open-data observation | Hungarian General Directorate of Water Management | 48.191, 19.53 | source | |
| Balassagyarmat | Hungary | 0.867 | Much below normal70% below the historic median | instantaneous | operational open-data observation | Hungarian General Directorate of Water Management | 48.076, 19.28 | source |
Related rivers
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.