What a Thermocline Is and Why It Ends Your Day

· 5 min read

What a Thermocline Is and Why It Ends Your Day

The layer that matters

By midsummer a deep lake stratifies into three layers. The warm upper layer holds oxygen. Below it sits a narrow band where temperature drops fast, and beneath that, cold water with almost no dissolved oxygen at all.

Fish cannot live in the bottom layer. If your electronics show fish at 40 feet and bait at 18, the fish are not at 40 feet.

Finding it

Watch for a hard clutter line on sonar. That is suspended plankton stacked on the density change. Fish the few feet above it, not below.

When it breaks

Fall turnover mixes the layers again and oxygen returns to depth. For a week or two the lake fishes badly, then it fishes better than it has since spring.

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