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How much does the lake warm or cool over the year? How does its oxygen level change? And how does its transparency and the development of algae fluctuate? To better understand its functioning, follow the evolution of the lake with the seasons.

Lake Geneva in summer

Separation into 3 superimposed water layers and algal development

In summer, the lake is divided into 3 superimposed water layers: the epilimnion (warm), the metalimnion (warm), the hypolimnion (cold).

The algae suspended in the water continue to grow in the epilimnion and metalimnion where they have sufficient light and nutrients (mainly nitrogen and phosphorus). The more algae there are, the less transparent the surface water becomes.

Algae are important to the functioning of the lake as they form the basis of the food chain. Most of them are not a problem, but some species are problematic: those that clog fishing nets, and toxic cyanobacteria.

The temperature of the waters of Lake Geneva in summer

In summer, the lake is divided into 3 layers of water. The epilimnion, located between the surface and about 10 m depth, is the layer which is almost homogeneous in temperature. Below, the metalimnion is the layer where the temperature decreases rapidly with increasing depth. It is located between 10 m and 30 m depth. Further down, the hypolimnion is the layer of cold water almost homogeneous in temperature located between the bottom of the metalimnion and the bottom of the lake. The metalimnion acts as a barrier and prevents the waters of the epilimnion and hypolimnion from mixing.


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Limnological bulletin

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

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