The site of the “Scientific Russia” project has published a large amount of material about Lake Glubokoe.
The water column of the lakes is divided into epilimnion, metalimnion and hypolimnion (“limnos” - Greek for “lake”), that is, into the upper layer of the lake, middle and lower. The boundaries of the layers are determined depending on the temperature of the water. In summer, the epilimnion is usually warm, with the same temperature throughout the layer. Only in its lower part does it decrease slightly. The epilimnion temperature in the middle of summer reaches 20-25 degrees. In the lower part of the lake (in hypolimnion), the temperature is also even, but very cold, within 5-6 degrees. At times it can be slightly lower.
In the middle part of the lake (metalimnion), the water temperature drops abruptly. In the upper part of this layer, it can be within 20 ° C (as in the epilimnion), and after 3-5 m - already 7-10 ° C, or even lower. So, for example, in Lake Glubokoe (Moscow region), the temperature drops from 20 degrees to 10 ° C.
On the shore of this lake there is a biological station “Glubokoe Ozero” (“Lake Glubokoe”), which was founded in 1891. All this time, hydrobiological work has been carried out there. It belongs to the A.N. Severtsov Institute of Ecology and Evolution of RAS.
By the middle of the warm summer, the thickness of the epilimnion reaches 5-7 m, the metalimnion - 3-7 m or more, depending on the heating of the water. The hypolimnion at the end of summer starts from 7-10 m and extends to the maximum depth. Lake Glubokoe has a depth of 32 meters.
28
June
2021