On 5 October 2026, the Rhine at Basel-Kleinhüningen recorded an exceptionally low daily discharge of 356 m³/s, part of the most severe low-flow sequence since 2020. These low water levels raise transport costs, degrade water quality, and restrict cooling, irrigation, and groundwater resources along the river.
On 5 October 2026, the average daily discharge of the Rhine at Basel-Kleinhüningen was lower than 1% of all measured daily discharges since 2020. The daily mean was 356 m³/s, with a minimum of 271 m³/s and a maximum of 457 m³/s. These values are exceptionally low for the date. The maximum discharge on 5 October ranked 21st over the last 30 days, 4th among all October days since 2020, and was also among the very lowest when compared with all days since 2020.
Over the past 30 days, the highest discharge was 576 m³/s on 8 September 2026, and the lowest was 188 m³/s on 22 September 2026. Table 2 lists the months with the lowest flow conditions since 2020; October 2026, with a minimum average flow of 356 m³/s, is the lowest on record for that period, followed by September 2026 at 361 m³/s. The current flow is therefore part of the most severe low-flow sequence observed in the available record.
Low water levels on the Rhine have consequences that reach well beyond the river itself. Cargo vessels have to reduce their load to stay clear of the riverbed, so more trips are needed to move the same volume and transport costs rise sharply, with the effect passed on to industries that depend on the waterway for coal, oil products, chemicals and grain. The shallower water also heats up faster in summer. Warmer water encourages bacterial growth, which can produce noticeable odors, and it holds less dissolved oxygen. The combination of higher temperatures, lower oxygen and more concentrated pollutants degrades water quality and can lead to fish kills. Swimming is generally discouraged under these conditions because of the higher bacterial load. Further effects include restrictions on power plants and industrial sites that draw river water for cooling, since they may no longer discharge warmed water without exceeding temperature limits, reduced dilution of treated wastewater, pressure on water supply and irrigation in the surrounding area, and falling groundwater levels along the river that affect riparian vegetation and wells.
| metric | '2026-10-05'::date | Historic |
|---|---|---|
| Average discharge | 356.3 | 894.1 |
| Maximum discharge | 456.5 | 2194.0 |
| Minimum discharge | 270.7 | 262.1 |
| Month | Min Avg Flow [m3/s] |
|---|---|
| 10.2026 | 356.3 |
| 09.2026 | 361.2 |
| 08.2026 | 413.0 |
| 08.2022 | 435.9 |
| 07.2026 | 442.1 |
🤖 This text was generated with the assistance of AI. All quantitative statements are derived directly from the dataset listed under Data Source.