Lake Geneva in winter

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Lake Geneva in figures

580 km2

Lake area

200.2 km

Length of the banks

309.7 m

Maximum depth

89 km3

Average volume

372 m

Average altitude
of the water body

11.3 years

Dwell time
theoretical waters

8,000 km2

Watershed area
from Lake Geneva*

1'400'847

Permanent population
in the watershed**

*The Lake Geneva watershed is the entire territory where surface water flows into Lake Geneva. It extends mainly across Switzerland (cantons of Vaud, Valais, Geneva and Fribourg) and France (departments of Haute-Savoie and Ain). It is fed by several rivers, including the Rhône , its main tributary, as well as the Arve, the Dranse, the Venoge and the Aubonne.

**Data for France: 2017 – Data for Switzerland: 2018

THE 4 SEASONS OF LEMAN

To what extent does the lake warm up or cool down over the year? How does its oxygen content change? And how does its transparency and algae growth fluctuate? To better understand how it works, follow the lake's evolution through the seasons.

Lake Geneva in winter

Winter mixing and end of algal development

In winter, lake water quality measurement campaigns return to a monthly schedule, as the development of algae in suspension in the water slows down. In fact, it's at this time of year that the surface waters are the most transparent.

Winter circulation adds oxygen to the lake by mixing oxygen-rich surface water with deep water, which contains less oxygen due to the decomposition of algae. In the case of a complete winter circulation, the oxygen deficit is fully compensated. In the case of repeated incomplete winter mixing, as has been the case since winter 2012-2013, the oxygen deficit at the bottom of the lake widens. At present, the lake lacks oxygen at depth, with adverse consequences for aquatic life and the release of phosphorus and certain metals trapped in the sediments.

Winter mixing also brings the nutrients needed for algae growth (mainly nitrogen and phosphorus) to the surface. But the cold, combined with low solar radiation, means that algae suspended in the water cannot develop immediately.

 

Lake Geneva water temperature in winter

Cold and windy spells mix surface water with deep water. Winter mixing is complete if the lake waters manage to mix all the way to the bottom. Otherwise, mixing is said to be incomplete. The more severe the winter, the greater the mixing depth.

Léman Live

Discover the fascinating real-time dynamics of the waters of Lake Geneva thanks to two innovative models, designed by researchers in the region, revealing the movements and temperatures of the lake.

Limnological bulletin

Discover the latest temperature, Secchi transparency, turbidity and chlorophyll a concentration measurement data and their evolution.

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