Kōrero: Lakes

Water circulation in a lake

Water circulation in a lake

During spring, summer and autumn, the upper layer (epilimnion) of a lake is warmed by the sun, and the wind keeps it well mixed and enriched in oxygen. The lower layer (hypolimnion) is cooler, and has less oxygen.

In winter the epilimnion cools, and there is complete mixing of all the water in the lake. Such annual mixing allows oxygen to be spread throughout the lake, and is an essential part of keeping the lake alive.

Te whakamahi i tēnei tūemi

Te Ara - The Encyclopedia of New Zealand

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Te tuhi tohutoro mō tēnei whārangi:

Simon Nathan, 'Lakes - Lake processes', Te Ara - the Encyclopedia of New Zealand, http://www.TeAra.govt.nz/mi/diagram/11817/water-circulation-in-a-lake (accessed 21 June 2024)

He kōrero nā Simon Nathan, i tāngia i te 24 Sep 2007