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In autumn, lake circulation can vary significantly depending on the lake's size, depth, and geographical location. Generally, as surface temperatures cool, the water becomes denser and can lead to mixing, known as turnover, where the colder, oxygen-rich water sinks and warmer water rises. This process enhances nutrient distribution and supports aquatic life, but the extent and timing of circulation can differ from one lake to another. Ultimately, the specific circulation dynamics in a given lake during autumn would require localized data for precise assessment.

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