3 main-stem GPS model cells · GloFAS v4
Feeds liveSeine · official main stem
The Seine on physical national-network gauges, ordered upstream to outlet on one shared profile axis. Side rivers drop in from above with the flow they deliver, each arrow landing on the water where it joins; reservoirs and their latest operator readings sit on the way down.
Loading gauge location map…
How reservoir releases reach the river
Water leaves the Seine through an intake canal and enters Lac d’Orient. A separate release canal returns stored water through two branches around Troyes. Diversion can reduce flow during floods; releases can support the river during dry periods.
Loading dated operator observations…
Operator explanation and latest daily bulletin. The daily bulletin may be newer than the GIS series used for this date-aligned comparison.
People, dams and institutions
Basin context loads as you approach this section.
Reference gauge: La Seine à Vernon - Station débitmétrique (>2006)144 m³/s · the furthest-downstream main-stem gauge currently reporting flow, so it captures the largest accumulated upstream reach.
Gauge coordinates and current discharge come from the named national hydrometric networks. The shared distance axis projects those GPS stations onto the dashboard’s sparse upstream-to-outlet spine; this is a profile axis, not surveyed navigation kilometre. The bed is interpolated between the dashboard’s anchor cells, because the registers on this river publish no gauge datum to draw it from. Where one register republishes another’s station, the two rows are one gauge and only the fuller record is plotted. River power is gravitational power carried by the flow (ρ·g·Q·Δh), not metered generation - it is a floor rather than a total, because a reach whose downstream gauge reports no discharge contributes nothing. The navigability line is an indicative planning threshold, not an official fairway forecast.